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banner announcing the 175th anniversary of the Astronomical Journal

The first issue of The Astronomical Journal (AJ) was published 175 years ago this month. This remarkable history means that the journal has persisted through the American Civil War and both World Wars, through 35 presidential administrations, and even through the development of “astronomer” as a profession in North America — it wasn’t until 50 years after the AJ’s launch that the continent founded its first professional society of astronomers, the American Astronomical Society.

As the first astronomy-focused academic journal to be published outside of Europe, the AJ has come a long way: its first issue — containing just a single printed article (“Development of the Perturbative Function of Planetary Motion”) — would have had limited circulation among the small but growing community of North Americans interested in astronomy. Now, as a fully open-access electronic journal, the AJ garners more than 100,000 views per year.

Early issues of the journal presented major advances in solar system and stellar science, laying the groundwork for modern discoveries in these fields. In the pages of the AJ, you can find foundational work establishing the ubiquity of black holes in the centers of galaxies, an examination of the iconic Hubble Deep Field, and Nobel-prize-winning evidence for the accelerating expansion of the universe, to name just a few works. Today, impactful observational results can be found alongside major advances in instrumentation, surveys, and software, such as the Wide-Field Infrared Survey Explorer, the Sloan Digital Sky Survey, and the astropy codebase.

To celebrate this remarkable milestone, we invite you to join us in looking back on the journal’s history using this interactive timeline. Here’s to 175 more years!

Io with a volcanic plume

Editor’s Note: This week we’ll be writing updates on selected events at the 56th Division for Planetary Sciences (DPS) meeting happening in Boise, Idaho, and online. The usual posting schedule for AAS Nova will resume on October 14th.

Table of Contents:


The Open-Source Science Initiative at NASA (J.L. Galache)

J.L. Galache (Agile Decision Sciences, NASA HQ) opened the session with a brief primer on open-science initiatives at NASA. Essentially, open science is the act of making your data, software, and publications freely accessible to all. Open science benefits the planetary science community by lowering barriers to entry and enhancing reproducibility of research. (Of course, open science also benefits you because your freely accessible data and publications will be cited more often!) NASA approaches open-science implementation through funding (sunpy and astropy have received funding from NASA, among many other recognizable names in science software), training, and policy. Current policy states that data and software should be made available at the time the research is published, and publications should be made available through a pre-print server (e.g., arXiv) if not being published in an open-access journal. Among the existing training options is Open Science 101, an online training module through which 1,900 people have already been accredited.

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Digging Deep: Unveiling Vertical Mixing and the Core Mass of Giant Exoplanets with JWST (David Sing)

David Sing (Johns Hopkins University), winner of the 2024 Alexander Prize for outstanding contributions that have significantly advanced our knowledge of planetary systems, described the journey to understanding exoplanet atmospheres and interiors from Hubble to JWST. Sing focused on the transit method, which has enabled the discovery of thousands of planets beyond our solar system and increasingly allows scientists to probe the atmospheres of those worlds.

With Hubble, scientists were able to test their models of photochemical equilibrium in exoplanet atmospheres, which predicted broad compositional trends with planet temperature. Hubble observations confirmed the basic picture of the chemical composition of hot Jupiters while also revealing complexities like clouds and hazes, which make it difficult to extract chemical abundances from spectra, and the presence of disequilibrium chemistry, which required extra attention from modelers.

plot of mass–metallicity relationship for planets and exoplanets

The mass–metallicity relationship for solar system planets (black points) and exoplanets (colored points). Click to enlarge. [From slide by David Sing]

Hubble observations raised further questions about giant planets, such as the state of their chemical disequilibrium, vertical mixing, horizontal mixing, and even their formation mechanism. Giant planet formation can be probed by measurements of planetary core mass fraction, with the core accretion model predicting that giant planets have roughly 10-Earth-mass rocky cores. In addition, the core accretion model predicts that as a planet’s mass increases, its overall metallicity decreases due to the accumulation of a massive envelope of hydrogen and helium. The giant planets in our solar system follow the predicted relationship, but the evidence for gas giant exoplanets is less clear. What can JWST tell us about the lingering issues in giant planet formation, chemistry, and mixing?

JWST spectrum of WASP-39b

JWST spectrum of WASP-39b’s atmosphere and best-fitting model. [From slide by David Sing]

Enter the JWST Transiting Exoplanet Community Early Release Science Program, which aimed to provide science results from phase curve, primary transit, and secondary eclipse observations of exoplanets while testing and leading to a greater understanding of the capabilities of JWST instruments. Sing highlighted the results of JWST transit observations of WASP-39b, which showed a prominent spectral feature from carbon dioxide (not seen by Hubble) as well as a feature at 4 microns that wasn’t predicted by models. This feature belonged to SO2, showing the first sign of photochemistry in an exoplanet. (SO2 is produced through the reaction of H2S with water molecules that have been split apart by starlight.)

Sing also described the important results from JWST observations of two other exoplanets, HAT-P-18b and WASP-107b. These are both cool/warm gas giants that are expected to have methane in their atmospheres. HAT-P-18b showed no sign of methane in its atmosphere — since the molecule is expected to exist, does this mean it’s being destroyed by photochemistry or by mixing into the deep, hot atmosphere of the planet?

Observations of WASP-107b provided more clues: in addition to CO2 and water, JWST observations of WASP-107b showed at last a hint of methane. However, there was about a thousand times less methane than expected given the planet’s temperature. By modeling both vertical mixing and photochemistry, Sing’s team showed that the methane depletion was due to mixing. Going further with these data, they used interior structure modeling to estimate the mass of the core at 11.5 Earth masses — consistent with predictions of the core accretion model.

Up next is the exoplanet grand tour spectroscopic survey, which will observe 25 exoplanets during 125 hours of JWST time. Stay tuned for news from this survey — the first data are being collected roughly 24 hours after this talk!

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Tracing the Heating of the Solar System Through Geochemical Signatures (Katherine de Kleer)

Katherine de Kleer (California Institute of Technology), winner of the 2024 Harold C. Urey prize for outstanding achievements in planetary science by an early-career scientist, described recent work on the history of heating in the solar system. De Kleer and collaborators use the Atacama Large Millimeter/submillimeter Array (ALMA) to understand where, when, and how objects in the solar system were heated and how that drives the chemical evolution of and geological activity on those objects today.

Let’s take things all the way back to the early days of the solar system: in the beginning, there was aluminum-26, a once-abundant, radioactive form of aluminum that heated the infant solar system. Heating from aluminum-26 melted early planetesimals and caused them to differentiate, separating into distinct compositional layers. Some of these planetesimals clumped together to form what are today the planets in our solar system, while others collided, leaving their remains scattered through the solar system as asteroids. The fragments of planetesimals in the asteroid belt can tell us about differentiation and, thus, heating in the protoplanetary disk that birthed our solar system.

thermal emission from asteroid Psyche

The thermal glow of asteroid 16 Psyche as seen by ALMA. [From slide by Katherine de Kleer]

Using ALMA, de Kleer observed the thermal emission from large main-belt asteroids — with an incredible resolution of 30 kilometers — and modeled the observations. The data show high emissivity (indicative of large metal content) but low polarization (indicative of scattering due to metal inclusions). This suggests that rather than having metal tied up in minerals, the metal in these asteroids likely exists in the form of numerous metallic chunks.

While heating is still ongoing in the solar system today, radiogenic heating — heating from the decay of radioactive material — is not as important as it once was. Now, small bodies are largely heated through tidal heating. The most dramatic example of the effects of tidal heating is Jupiter’s moon Io — the most volcanically active body in the solar system. Tidal heating melts Io’s rocky interior, which then gushes through the moon’s 400 active volcanoes to its surface.

Many images of Io and its volcanoes

Many views of the infrared glow of Io and its many volcanoes. Wavelength increases toward the bottom. Click to enlarge. [Slide by Katherine de Kleer]

By studying when and where Io’s volcanoes erupt, de Kleer’s team hopes to learn about Io’s interior, including where tidal heating is deposited. Tidal heating models predict specific distributions of Io’s volcanoes, but after 300 nights of observing Io (covering many revolutions around Jupiter), there doesn’t appear to be any cyclical behavior to the eruptions, nor does the spatial distribution appear to match the models well. This could mean that convection in Io’s mantle is obscuring the signature of tidal heating, or there could be stochastic geological processes at play.

Scientists have studied volcanic activity on Io for forty years, but the moon has been active much, much longer. If Io has been trapped in a resonance with fellow moons Europa and Ganymede for billions of years, as research suggests, it must have lost the equivalent of its entire mantle contents many times over, churning through and reprocessing this mantle material repeatedly. Another way of looking at Io’s evolution over time is through its atmosphere. Sulfur — an abundant component of Io — is lost to space from the moon’s upper atmosphere. Because different isotopes of sulfur have different masses, lighter isotopes are held less tightly to the moon and are preferentially removed from the atmosphere. By measuring the ratio of different isotopes of sulfur, de Kleer showed that Io has lost 94–99% of its available sulfur, supporting the picture of a dramatically, dynamically heated and evolving world.

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JWST image of Uranus and its moons

Editor’s Note: This week we’ll be writing updates on selected events at the 56th Division for Planetary Sciences (DPS) meeting happening in Boise, Idaho, and online. The usual posting schedule for AAS Nova will resume on October 14th.

Table of Contents:


Plenary Lecture: Addressing Mental Health in Planetary Science: Big and Small Steps to Creating an Environment that Supports Well-Being (David Trang)

Planetary scientist and mental health counselor David Trang (Space Science Institute) discussed the results of recent surveys of mental health among planetary scientists and strategies to improve the health of the community. Mental health is a pressing issue for our community: 76% of planetary scientists surveyed reported having anxious or depressive symptoms that made it at least somewhat difficult to perform work duties, take care of things at home, or get along with others. Twenty-nine percent of respondents found these tasks difficult, while 9% of respondents said they found these tasks very difficult.

These issues affect everyone: even if you’re not personally experiencing symptoms, the collaborative nature of planetary science means that someone you work with likely is. Distracting thoughts associated with anxiety, stress, and depression occupy short-term memory, affecting research quality, the ability to develop new ideas, interpret data, and more. Aside from research quality, poor mental health worsens physical and social health as well.

results of survey of anxiety among planetary scientists

Prevalence of clinically significant anxiety among planetary scientists in 2022 and 2023. Rates are compared against the general population during (red line) and before (green line) the COVID pandemic. Click to enlarge. [Slide by David Trang]

To examine the mental health of our community, Trang surveyed roughly 300 planetary scientists in 2022 and 2023, using common anxiety, stress, and depression assessments. The survey indicated higher than average anxiety and depression among female, POC, LGBTQ+, and early career respondents. Notably, graduate students had the highest prevalence of anxiety and depression of any of the groups surveyed. While stress, anxiety, and depression decreased for nearly all demographic groups in 2023 compared to 2022, even after decreasing to 2023 levels, planetary scientists across the board remained more stressed, anxious, and depressed than the average respondent from the general public, pre-COVID. For almost all groups, levels remained higher among planetary scientists in 2023 than the general population during the peak of COVID.

Overall, the results show a statistically significant difference in the prevalence of anxiety, stress, and depression between members of marginalized groups and members of non-marginalized groups. While this difference may reflect larger cultural and societal issues, it also presents an opportunity for planetary science participation to become a protective factor against these larger issues.

survey results showing differences in depression and anxiety between mission participants and non-participants

Prevalence of clinically significant anxiety and depression among mission participants (purple) and non-participants (blue). The white shapes indicate statistically significant results. Click to enlarge. [Slide by David Trang]

In what way might the planetary science community be protective? As an example, Trang showed that there are statistically significant differences in the prevalence of anxiety and depression between scientists that participate in missions and those that do not. Why mission participation has a protective effect isn’t yet clear, but Trang hypothesized that mission participation creates a sense of belonging to a group, and it also pairs early career scientists with a larger number of potential mentors, increasing the chances of there being a positive mentor relationship. (During the Q&A, audience members proposed other potential factors, such as stability of funding and the impact of working toward a common goal.)

To bring these positive aspects of mission participation to all planetary scientists, Trang suggested creating more teams (not just missions, but research institutes and interest groups as well) and improving mentorship for early career scientists. To achieve the latter goal, institutions could implement mandatory mentorship training for graduate advisors or invest in a mentor advisor to provide career mentorship to a large number of graduate students, reducing the burden on graduate research advisors.

plot of top contributors to depression

Top contributors to depression. Click to enlarge. [Slide by David Trang]

In addition to these larger policy changes, individuals can make small changes that have a big impact. One area of focus is expressing appreciation, as many of those surveyed said that not feeling appreciated was a major contributor to their anxiety or depression. Trang suggests that simply saying thank you with one sentence explaining why you’re grateful can go a long way. And as someone receiving an expression of appreciation, be sure to say how you felt about it (e.g., “You’re so welcome, I’m happy to hear that you found it helpful!”) — this makes it a positive experience for everyone involved.

Trang presented two other strategies that can help people feel appreciated: focusing on strengths and complimenting the process. As scientists — especially scientists in advisor roles — it’s easy to focus on what’s wrong and what needs improvement. For example, when editing a student’s manuscript, it’s natural to point out what needs to be fixed. But don’t forget to focus on what’s been done well (e.g., “You did a great job of reviewing past work in the introduction. Let’s bring that same strategy to the discussion section.”). Similarly, it’s easy to congratulate or compliment someone after a major achievement — say, being awarded a grant — so try to compliment the steps of the process as well. For example, take the time to acknowledge the hard work that went into writing an excellent proposal, even if it wasn’t selected.

Want to implement these changes in your life? Set SMART goals, Trang suggests. Give yourself a Specific, Measurable, Achievable, Relevant, Time-bound goal, such as pointing out two strengths each time you review a paper this year. Through individual efforts and broad policy changes, we can make the planetary science community a healthier place.

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Press Conference: Amy Simon, Richard Cartwright, Mariah Jones (Briefing video)

First to speak was Amy Simon (NASA’s Goddard Space Flight Center), who presented results from a long-term study of Jupiter’s Great Red Spot. The famous Great Red Spot is the largest storm in the solar system, spanning 10,000 miles (~16,000 km). Although it’s been a constant feature of Jupiter’s disk for centuries, it’s both steadily shrinking and changing in more subtle ways. Simon’s team used the Hubble Space Telescope to investigate the Great Red Spot’s 90-day oscillations, which are periodic changes in the rate at which the storm drifts westward. This rate oscillation is seen in historical and ground-based data. The Hubble observations showed that many aspects of the spot varied over the course of 90 days. The spot’s semimajor axis varied, though it’s north–south extent did not, and the height and width of the deep-red core changed.

Great Red Spot with regions labeled

Regions of Jupiter’s Great Red Spot. [From slide by Amy Simon]

All of these changes were roughly in phase with one another. Other changes, such as changes to the reflectance of the core of the spot and the collar region just outside the core, were out of phase with each other. Some parameters were also correlated, such as the spot’s size and speed; the spot is largest when it is moving most slowly. The core is also brightest when the spot is largest, although this change is small. An analysis of the wind velocity field showed that the surrounding velocity isn’t compensating for the other oscillations. This indicates that a simple two-dimensional model in which changes in vorticity balance the oscillations doesn’t apply to this system, and the three-dimensional atmospheric structure must be more complex.

Uranus's moon Ariel

Ariel as seen by Voyager 2 in 1986. [NASA/JPL]

Next, Richard Cartwright (Johns Hopkins University Applied Physics Laboratory) brought things farther out in the solar system with new JWST observations of Ariel, the fourth-largest moon of Uranus. The JWST data revealed the presence of CO2 and CO ice on the moon’s surface. This finding is intriguing because these materials likely escape to space over time, so they must be replenished somehow. CO2 ice might form via irradiation of materials on the moon’s surface by energetic particles trapped in Uranus’s magnetosphere. The alternative, which is favored by the JWST data, is that CO2 gas could escape from a reservoir below the surface and condense on the surface.

JWST spectrum of Ariel

JWST observations of Ariel. The spectra show clear signals from CO2, CO, and H2O, plus a tentative hint of CO3. Click to enlarge. [From slide by Richard Cartwright]

A potential reservoir could be a subsurface ocean rich in CO2, CO, and possibly CO3. If CO3 were to be found on Ariel’s surface, that would be strong evidence for the presence of such an ocean, since it’s a difficult compound to make on the surface of an airless body. The JWST data show a tiny hint of a CO3 feature as well as a feature that could be interpreted as being due to clathrates — chemical lattices that trap molecules. Both of these features, if confirmed, would provide firm evidence for the subsurface ocean hypothesis. Curiously, the data show no hint of hydrogen peroxide, which has been seen on the moons Europa, Ganymede, Enceladus, and Charon. This might hint that the radiation environment at Ariel is quieter than expected.

Future work will dive deeper into new JWST observations of Uranian moons Umbriel, Titania, and Oberon. Preliminary analysis of the JWST spectra shows the first evidence of CO ice on these worlds.

simulation results for simulated co-orbitals in exoplanet systems

Comparison of the results for TRAPPIST-1 (top), a resonant system, and Kepler-90 (bottom), a non-resonant system. More of the synthetic co-orbitals remained in stable configurations in the Kepler-90 system. Click to enlarge. [From slides by Mariah Jones]

Finally, Mariah Jones (Vassar College/SETI Institute) took things out of the solar system altogether with a theoretical exploration of co-orbiting bodies in exoplanet systems. Co-orbitals are bodies that share an orbit. For example, the Jupiter trojan asteroids share Jupiter’s orbit. Trojans are a class of co-orbitals that sit 60 degrees in front of and 60 degrees behind a planet. Horseshoes are co-orbitals with a more complex configuration, librating around 180 degrees from their host planet. In our solar system, Mars, Jupiter, and Neptune host stable populations of co-orbiting bodies, but Saturn and Uranus do not. The reason for this may be that Saturn and Uranus are both in near-resonance with Jupiter and Neptune, respectively. Orbital resonance refers to a setup in which the orbital periods of two or more bodies are integer multiples of one another.

Jones and collaborators used dynamical modeling to investigate if the presence of resonance in a planetary system affects the long-term stability of co-orbital populations. They collected initial conditions for several multi-planet systems from the NASA Exoplanet Archive and injected 20 synthetic co-orbitals into each system. They found a variety of behaviors, including stable trojans and horseshoes, no stable solutions, or switching between stable trojan and horseshoe configurations. They found that stable configurations were more likely for systems without resonance. This trend might happen because in a resonant system, bodies that are co-orbital with one planet are also in resonance with another planet, destabilizing the configuration.

Slides from these three presentations are available in the press kit.

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Titan and Saturn

Editor’s Note: This week we’ll be writing updates on selected events at the 56th Division for Planetary Sciences (DPS) meeting happening in Boise, Idaho, and online. The usual posting schedule for AAS Nova will resume on October 14th.

Table of Contents:


Plenary Lecture: Planetary Habitability in the Solar System and Beyond (Stephen Kane)

What is planetary habitability? This deceptively simple question posed by Stephen Kane (University of California, Riverside) is surprisingly controversial. Kane defines the answer as an assessment of the energy balance at a planet’s surface and what influences that balance over time. When looking at the vast sample of exoplanets — nearly 6,000 are currently known — Earth-size planets are common, opening up the possibility that the circumstances necessary for habitability are common as well.

image of Venus featuring swirling clouds

Venus as seen by the Mariner 10 spacecraft. [NASA/JPL-Caltech]

But the problem is a tricky one. Take Venus, for example. To a distant observer, Venus and Earth are both “Earth-like” planets, but only Earth is habitable today. The differences between the two are many — Venus is 30% closer to the Sun and receives twice the solar flux, and it also lacks a moon, rotates extremely slowly and nearly perfectly upside down, lacks a magnetic field, and lacks plate tectonics — but it’s not yet clear which of these properties are responsible for the hellish conditions on Venus today. Time is also an important factor: as recently as a billion years ago, Venus may have had surface water.

Water is a recurring theme in discussions of habitability, since one framework within which to assess a planet’s energy balance is whether a planet is able to sustain liquid water on its surface. This framework is reasonable — and not unreasonably Earth-centric — because water is common throughout the universe, it’s a solvent in which biochemical reactions can take place, and it remains liquid up to (relatively) high temperatures, allowing chemical reactions necessary for life to proceed quickly.

graphic listing the many factors important for planetary habitability

The multitude of factors that could impact planetary habitability. What this graphic doesn’t show — and what’s critical to find out — is the relative importance of these factors and the connections between them. Click to enlarge. [Slide by Stephen Kane; originally from Vicky Meadows and Rory Barnes]

There are many interconnected factors that play a role in determining a planet’s energy balance, and it’s challenging to understand which are most important. To approach this problem, Kane suggests using the “statistical hammer” of exoplanets and taking cues from our own solar system’s evolutionary history. As an example of what we can learn from our own solar system, Kane pointed to Mars, which has an interesting habitability history. Mars has been examined closely by the Mars Atmosphere and Volatile EvolutioN (MAVEN) mission for a decade, and MAVEN measurements show that Mars once had a surface pressure similar to present-day Earth. Today, Mars has lost much of its atmosphere, rendering the planet cold and dry.

Atmospheric loss is important when considering exoplanets as well. In the TRAPPIST-1 system, which is famous for containing seven terrestrial planets, three or four of which are in their star’s habitable zone, recent JWST observations suggest that the two planets closest to the star have little to no atmosphere. (A hazy or cloudy atmosphere is possible for TRAPPIST-1 c, but TRAPPIST-1 b is extremely unlikely to have any kind of atmosphere.)

Another consideration for exoplanetary systems is the presence or absence of giant planets. Our solar system may be unusual among planetary systems because it contains four giant planets beyond the snow line (the distance from the Sun at which water exists as ice). Many other known exoplanet systems contain giant planets closer to their stars, which may prevent Earth-size planets from attaining stable orbits in the habitable zone. However, a well-placed giant planet may be critical for the habitability of Earth-like planets; giant planets positioned beyond the snow line can transport volatiles (critically, water ice) into the inner solar system. While Jupiter has a nearly circular orbit, researchers see giant planets beyond the snow line with a wide range of orbital eccentricities — and it turns out that giant planets with more elliptical orbits are actually better at scattering volatiles toward would-be Earths.

In the conclusion, Kane added a rather somber comment about the challenge of assessing planetary habitability: modeling suggests that the three biggest factors determining Venus’s current uninhabitability are the incident solar flux, Venus’s slow rotation rate, and its lack of plate tectonics. A distant observer could easily pin down the first of those three factors, but the other two are difficult or impossible to determine from afar.

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Plenary Lecture: From Venus to Exoplanets and Back Again (Cedric Gillmann)

Cédric Gillmann (ETH Zurich) brought the discussion back to Venus in the second talk of the session. Seen from afar, it would be very difficult to distinguish Venus from Earth because the two planets have similar basic properties. This fact led Venus to be a prominent target of early solar system exploration, with some observers expecting Venus to be a sort of warm and humid “space Florida.” Instead, images from the surface revealed Venus to be dry and lifeless, though more Earth-like than it seemed at first glance: the images showed basaltic (composed of volcanic rock) plains similar to those found on Earth.

That might be where the similarities between Venus and Earth end. Though Venus and Earth both have volcanoes, the type and distribution of volcanic features is dissimilar, suggesting that something in Venus’s interior is markedly different from Earth’s. Venus also has a staggeringly high surface pressure (more than 90 times Earth’s surface pressure) and temperature (hot enough to melt lead) and an atmosphere rich in carbon dioxide, with some nitrogen and just a trace of water.

Comparison of known Venus zone and habitable zone planets

Comparison of known Venus zone and habitable zone planets. [Slide by Cédric GIllmann]

Much remains unknown about Venus. Observations suggest that the planet has lost much of its atmosphere, but it’s not yet clear how much was lost and when. Luckily, several missions to Venus are in preparation that will help researchers learn more about our neighboring planet — and about exoplanets as well. Given the bias toward finding short-period exoplanets, we know of more planets in the “Venus zone” than in the habitable zone. By studying Venus, we can learn more about these Venus-zone exoplanets that we’ll never be able to observe at close quarters.

This is just one example of how exoplanet studies increasingly benefit from solar system studies. Certain factors, especially those related to planetary interiors, can never be measured directly for exoplanets but can be investigated for solar system planets. Gillmann pointed to the mantle as an especially important factor; as a planet’s mantle evolves, it affects the planet’s core and cools the planet. It also affects volcanism, which in turn affects the planet’s atmosphere, making it central to the planet’s overall evolution.

In summary, Venus represents a planet whose evolutionary history is likely complicated and is still uncertain, though upcoming missions like EnVision and VERITAS should help to illuminate its past. By studying the relatively accessible Venus, astronomers can learn more about planets that we’ll never get to see up close.

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Plenary Lecture: ExoTitans: Connecting Solar System and Exoplanet Studies (Kathleen Mandt)

In the final talk of the session, Kathy Mandt (NASA’s Goddard Space Flight Center) took the habitability discussion in a colder direction, whisking the audience to the ocean worlds of the outer solar system. Our solar system contains several moons with liquid oceans beneath their icy surfaces. The Europa Clipper mission, which is scheduled to launch no sooner than 12 October, will explore one of these ocean worlds in detail.

Ocean worlds are an enticing place to look for life beyond Earth, but it’s exceedingly difficult to study the oceans directly. It’s unknown how thick the ice shells may be, and even drilling through antarctic ice on Earth is difficult. This means that studying the subsurface ocean on an exoplanet will be beyond our reach. Is there an easier way to study exoplanet ocean worlds?

Titan's polar seas

Radar image of Titan’s north polar seas. [NASA/JPL-Caltech/ASI]

Saturn’s largest moon, Titan, may be the best place to start to learn about exoplanet ocean worlds. Titan has a thick atmosphere composed mainly of nitrogen and methane, which react to form complex hydrocarbons and nitriles, creating haze. It also has a multitude of lakes and seas filled with a freezing, oily mixture of liquid methane and ethane. There are 130 recorded flybys of Titan by the Cassini spacecraft, providing ample data to compare to exoplanet observations.

Titan-like exoplanets are likely to be common, but our current detection capabilities limit the number of candidate exo-Titans — because these planets must be cold, they must be located farther from their stars, making them harder to detect with the transit method.

illustration of the TRAPPIST-1 planets

An artist’s rendition of the seven known planets in the TRAPPIST-1 system, based on data taken through 2018. [NASA/JPL-Caltech/R. Hurt, T. Pyle (IPAC)]

One candidate exo-Titan is TRAPPIST-1 h, the outermost of the known TRAPPIST-1 planets. Based on its bulk density, TRAPPIST-1 h’s water-to-rock ratio is higher than Earth’s but lower than Titan’s, placing it somewhere around Europa. TRAPPIST-1 h may have cryovolcanoes, and climate modeling shows that while it’s too warm for liquid methane — a critical component of Titan’s hydrocarbon seas — it’s the right temperature for liquid ethane.

If TRAPPIST-1 h is an exo-Titan, what would JWST enable us to learn about its atmosphere? Mandt’s team performed atmospheric modeling of exo-Titans to estimate what JWST would see when looking at such a planet. They found that it was often difficult to back out the input properties of a planet since there was a lot of degeneracy between temperature and pressure. Some factors, such as eddy diffusion, were impossible to discern at JWST-accessible infrared wavelengths but could be probed by an ultraviolet telescope.

Next, Mandt’s team plans to incorporate more complex photochemistry in their model, which will likely be challenging. TRAPPIST-1 is an M dwarf, which means that the star is variable at the X-ray and ultraviolet wavelengths that drive chemical reactions.

Ultimately, Mandt emphasized the importance of planetary scientists and exoplanet scientists working together, leveraging past knowledge from Cassini and upcoming insights from the Dragonfly mission to interpret observations of exo-Titans and other ocean worlds.

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image of Europa

Editor’s Note: This week we’ll be writing updates on selected events at the 56th Division for Planetary Sciences (DPS) meeting happening in Boise, Idaho, and online. The usual posting schedule for AAS Nova will resume on October 14th.

Table of Contents:


Press Conference: Quanzhi Ye, Elizabeth Silber, and Victor Oyiboka (Briefing video)

The first of two press conference sessions at this year’s DPS meeting featured research regarding small bodies and planets of the inner solar system. First up was Quanzhi Ye (University of Maryland/Boston University), who described a search for potentially hazardous asteroids in the Taurid complex. The Taurid complex is a collection of debris from comet 2P/Encke, which descended from a parent body some 10,000–20,000 years ago. The size of the parent body is unknown but may have been as large as 100 kilometers across. When Earth passes through the debris left behind by this comet, observers on the ground see a meteor shower. Unlike better-known meteor showers like the Perseids, the Taurids aren’t particularly active, but they are unusually rich in large particles that create dramatic fireballs when they burn up in Earth’s atmosphere.

The Taurids have been known for a century, and a significant year-to-year variation in the activity level has become apparent. This variability happens because some of the Taurid complex is trapped in a resonance with Jupiter (these trapped particles are called the Taurid resonant swarm); when Earth passes close to the center of these trapped particles, the activity level is particularly high. While most of the trapped Taurid particles are tiny, the resonant swarm may also contain asteroids 100 meters wide or larger that have been trapped by Jupiter’s gravity. This means that when Earth passes close to the center of this particle swarm, it could be passing close to potentially hazardous asteroids — but how many hazardous asteroids are actually there?

To answer this question, Ye and collaborators analyzed data from the Zwicky Transient Facility during two recent encounters with the Taurid swarm. They found no trace of potentially hazardous 100-meter-plus asteroids — phew! The non-detection suggests that there are only 9–14 asteroids this large in the Taurid swarm. This is tiny compared to the 3,000 or more known potentially hazardous asteroids. These observations also allowed the team to estimate the size of the comet 2P/Encke parent body at just 10 kilometers, which is smaller than previously thought.

Next, Elizabeth Silber (Sandia National Laboratories) discussed a topic of importance to planetary defense. Earth is constantly being bombarded with debris, and while most of this debris is extremely fine and poses no threat to us, larger objects can be destructive. Large meteoroids (objects up to 1 meter in diameter) and asteroids (objects larger than 1 meter in diameter) can generate shock waves that can be felt on the ground and can damage property and cause injuries. For example, in 2013, the house-sized (18-meter-wide) Chelyabinsk meteor exploded with an energy equivalent to 440 kilotons of TNT and shattered thousands of windows.

cartoon showing different types of meteors and their light curves and infrasound measurements

Demonstration of how the properties of a meteor are reflected in light curves and infrasound measurements. Click to enlarge. [From slide by Elizabeth Silber]

In order to predict destructive events like these, it’s important to be able to characterize asteroids. This can be done using a variety of ground- and space-based techniques. Silber focused on the measurement of asteroidal impact energy with infrasound: low-frequency sound below the threshold of human hearing. Infrasound detectors provide a powerful way to study asteroids because they can be deployed in remote areas and can work night and day and in essentially any weather conditions.

Silber’s goal was to develop a practical way to estimate an asteroid’s impact energy — and eventually size and velocity — which will help to assess future threats. The team combined a sample of infrasound measurements with other measured asteroid properties and light curves to assess the reliability of the infrasound technique. Ultimately, this work will aid in determining the rate at which asteroids of various sizes impact Earth’s atmosphere and the level of risk associated with asteroids of different sizes.

Finally, Victor Oyiboka (University of Texas at Dallas) introduced new work on the role of radioisotopes on the evolution of Earth-like planets. Radioisotopes are radioactive forms of elements. Essentially, these are unstable atoms that split into more stable forms and release energy. As radioactive isotopes in a planet’s interior decay into more stable forms, the energy released heats the planet, helping to shape its evolution.

plot of heat production as a function of planet age

Model results for the heat production of Earth-like exoplanets as a function of planet age. [From slide by Victor Oyiboka]

Oyiboka and collaborators used the properties and half-lives — the time it takes for half of a radioactive sample to decay — of several critical radioisotopes to model the amount of radioactive heat produced by an Earth-like planet as a function of time after the formation of the galaxy and the planet’s age. For Earth, the most important radioisotopes were initially aluminum-26, which provided the bulk of the internal heat to the young Earth, and iron-60. These short-lived isotopes have long since decayed, leaving behind long-lived isotopes like potassium-40, thorium-232, uranium-235, and uranium-238 that still exist today. The team’s calculations gave them an estimate of the heat produced internally, which they then converted to a flux of heat through the planet’s surface. These estimates will be useful for studies of planetary evolution and habitability.

Slides from these three presentations are available in the press kit.

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Plenary Lecture: Laboratory Investigations Toward Understanding Ocean World Surfaces (Tuan Vu)

The first of four plenary sessions at this year’s conference introduced laboratory experiments relevant to planetary science. First was Tuan Vu of NASA’s Jet Propulsion Laboratory, who described laboratory work that explores the salts and ices that might be found on some of the ocean worlds in our solar system. Ocean worlds — planetary bodies with surface or subsurface oceans — are potential habitats for life beyond Earth and are therefore of great interest to planetary scientists. Among our solar system’s ocean worlds are Jupiter’s moon Europa, which likely contains twice as much water as Earth, and Saturn’s tiny moon Enceladus, which despite its small size may contain 14–20% as much water as Earth. These moons’ subsurface oceans are thought to be salty and chemically complex, and knowing the composition of these worlds’ oceans is critical to understanding their geochemistry and habitability.

Vu focused on Europa, which is soon to be visited by the Europa Clipper mission. Unlike Enceladus, which frequently broadcasts the contents of its ocean via plumes that erupt from fissures in its surface, Europa only rarely emits plumes. This means that researchers will likely need to glean the composition of Europa’s oceans by studying its surface, which may be spotted with frozen brine from infrequent plumes or ocean material welling up through cracks in the ice shell. The first challenge for this tactic is measuring the composition of the surface. Then, researchers must translate the composition of ices on the surface to the composition of liquids in the moon’s ocean by determining how ocean materials will be altered by deposition on the surface and exposure to the intense radiation environment.

Observations from ground-based telescopes, the Hubble Space Telescope, and the Galileo spacecraft have found evidence for sodium chloride (NaCl), sodium- and magnesium-containing minerals, and sulfates on Europa’s surface. Vu’s team created laboratory brines from sodium, chloride, magnesium, and sulfate ions and observed the minerals that formed under different ion concentrations, ion ratios, and freezing rates. These experiments showed that mirabilite (NaSO4) preferentially forms over epsomite (MgSO4) even when magnesium ions are abundant. However, epsomite has been observed on Europa, with sodium instead latching on to chlorine to form NaCl. This combination cannot be achieved by the simple freezing of ocean materials. Instead, it requires an ocean rich in NaCl and a surface that is bombarded by ionizing radiation, further processing the ocean materials after they reach the surface and freeze.

plot of surviving colony forming units under different experimental conditions

Colony forming units (CFU) of Pseudoalteromonas haloplanktis bacteria after exposure to ambient conditions, vitreous salt hydrate, and crystalline salt hydrate. [From slide by Tuan Vu]

Considering the effect of freezing rate, Vu’s team found that flash freezing creates glassy, amorphous blobs of frozen brine rather than sharply defined crystals. These glassy structures appear to be highly stable — in other words, they’re unlikely to crystallize over time. This has a couple of interesting implications: first, amorphous (otherwise known as vitreous) salt tends to have fewer spectral features than crystalline salt. (Here, salt is used in the chemical sense to mean a compound made from positive and negative ions; table salt — sodium chloride — is just one example of a salt.) This means that if future missions to Europa find unexpectedly bland surface spectra, amorphous salt may be to blame. Second, amorphous salt is less likely to damage cellular structures when freezing than crystalline salt. This has important consequences for the search for life on Europa. To investigate this finding further, Vu’s team acquired a bacterium that is found in antarctic seawater — which is both cold and extremely salty — and brought samples of bacteria down to 100K (roughly the temperature of Europa’s surface) in the presence of amorphous or crystalline salt. Remarkably, many of the bacteria survived the journey to freezing and back, with the amorphous sample faring better than the crystalline sample.

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Plenary Lecture: The Next-Generation Laboratory Experiments on Planetary Materials (Xinting Yu)

Certain worlds in the solar system can appear deceptively Earth-like while being completely alien. Such is the case for Saturn’s largest moon, Titan, which sports familiar-looking seas, clouds, and dunes. Xinting Yu (University of Texas at San Antonio) was introduced to materials science via Titan’s curiously Earth-like dunes. Earth’s dunes are primarily made of quartz, while Titan’s dunes are made of organic material.

Yu and collaborators initially attempted to study Titan-like dunes in a wind tunnel using ground walnut shells and coffee grounds as a stand-in for the dune material. However, these materials were a poor analog, leading the team to explore tholins as an option. Tholins are a class of molecule thought to exist in Titan’s ever-present haze layer. They can be created by adding energy to a mixture of nitrogen and methane. While tholins excel at imitating organic compounds on Titan, they’re also toxic and time-consuming to make. (In three days, the team generated just one gram of the 2–3 kilograms they needed for the wind tunnel.) Instead of going this route, Yu’s team studied the material properties of Titan’s dunes and used these properties to scale the wind tunnel data.

This experience led Yu to bring materials science techniques to planetary science questions. With the Dragonfly mission expected to touch down on Titan (on the dunes, in fact!) in 2034, materials-science-inspired studies of Titan are timely. Recently, Yu’s planetary materials lab has sought to answer two pressing questions: 1) does the fact that lab-made Titan materials are prepared in air that contains oxygen and water vapor — two things absent from Titan’s atmosphere — affect their properties, and 2) are the tholins made in labs really like the tholins on Titan?

plot of total surface energy of lab-generated tholins

Demonstration of how the total surface energy of lab-generated tholins changes with the chemical mixture used to make them (represented by the color of the bar) and the experimental setup (labeled on the horizontal axis). Click to enlarge. [From slide by Xinting Yu]

To answer the first question, Yu’s team devised a method to create tholins without ever letting them touch Earth air. As it turns out, exposure to Earth’s atmosphere completely changes the material. To answer the second question, Yu’s team first collaborated with other Titan-materials labs to compare the properties of tholins created in different labs. While the lab setups used to create the samples were all different, they were transported, stored, and analyzed the same way. This study showed that the largest determining factor in the surface energy (a measure of the “stickiness” of the molecules, which impacts their behavior) of tholin samples is the experimental setup. This study also allowed the team to show that tholin samples energized with cold plasma rather than ultraviolet light provided the best match to existing Titan cloud observations.

Yu’s team has put together a database of these materials for anyone wanting to study Titan. Yu closed the talk with a video tour of the Planetary Material CHaractErization Facility (PMCHEF) and a reminder than tholins aren’t just relevant to Titan — hazes are thought to be common in exoplanets, and laboratory studies can help researchers peer into those planets’ atmospheres as well.

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Plenary Lecture: Spectroscopy of Fine-particulate Minerals in the Laboratory and the Field: A TREX Perspective (Melissa Lane)

Melissa Lane (Fibernetics) closed out the session with a two-part talk that covered spectral characterization of mineral dust and investigation of rover techniques. In order to interpret spectra of distant planets, researchers need to be able to refer to laboratory spectra of common planetary materials. Lane’s team’s goal was to collect far-ultraviolet to mid-infrared laboratory spectra of 27 types of mineral dust. Why study dust? Dust is ubiquitous in the solar system, coating geological features of interest and interfering with human and robotic exploration.

Example Frankenspectrum of olivine

Example Frankenspectrum of olivine. [Slide by Melissa Lane]

The team created samples of finely ground minerals and distributed them to several labs for analysis. Using a variety of setups, the labs returned spectra of the materials over different wavelength ranges, which Lane and collaborators scaled, adjusted, and stitched together to create a single “Frankenspectrum” for each mineral. All 27 Frankenspectra are available on the Planetary Data System along with the original, unadjusted spectra. While the Frankenspectra have limitations — Lane notes that they weren’t collected under vacuum conditions, which means that the mid-infrared portions of the spectra aren’t appropriate for comparing to spectra of airless bodies — this study goes a long way toward providing an extensive library of reference spectra for planetary studies.

Lab spectra are also important for guiding autonomous robotic exploration of planetary worlds. In the second portion of the talk, Lane’s team used the Zoë rover to explore the outcomes of different rover mission architectures: 1) autonomous rover, 2) traditional remote-team-guided rover, and 3) astronaut and semi-autonomous rover. The team traveled to Yellow Cat, Utah, and to the Hopi Buttes volcanic field in northern Arizona, both of which have a variety of geologic features. They found that while the autonomous rover was the fastest, it missed things that the human-guided scenarios caught.

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logo of the American Astronomical Society

AAS Director of Scholarly Publishing Kerry Kroffe

AAS Director of Scholarly Publishing Kerry Kroffe [Nick Leoni]

Last month, Kerry Kroffe joined the AAS staff as Director of Scholarly Publishing. While Kerry may be new to the AAS staff and to many members of the AAS community, he and the AAS journals go way back — read on to learn about Kerry’s journey to his present role and his goals for the AAS journals publishing experience.

The Path to the AAS

After his first publishing role with a for-profit book publisher, Kerry joined the staff at the University of Chicago Press working as the Assistant Publication Manager for the AAS journals in 2000. Working with former AAS CEO Bob Milkey and current CEO Kevin Marvel, he found that the AAS journals embodied a publishing ethos that spoke to him — rather than a for-profit model that endlessly seeks to maximize profit at the expense of the contributors or the audience, the AAS staff sought to be good stewards of the literature, and to serve the authors and the readers.

“I’ve worked with medical professionals, biopharm, all sorts of groups out there, and I’ve honestly just not found a community that I resonate with as much as the astronomers,” Kerry says.

Kerry Kroffe photographed at Grand Canyon National Park

In addition to thru-hiking, Kerry’s also a fan of national parks — he’s hiked in 27 of them, including Grand Canyon National Park, seen in the background here. [Kerry Kroffe]

When the AAS journals portfolio transitioned publishers from the University of Chicago Press to the Institute of Physics (IOP) Publishing in 2008, Kerry followed. He shepherded AAS journals articles through the publishing process at IOP until 2014, when he planned to undertake a thru-hike of the 2,200-mile Appalachian Trail. But the trail would have to wait — having already told IOP his plans to depart several months in the future, Kerry got an offer he couldn’t refuse: to work at the Public Library of Science (PLOS), a nonprofit open-access science publisher.

“It had always been a dream of mine to work at PLOS,” Kerry says. “I loved what they stood for.” At PLOS, he was responsible for all of the editorial operations — everything on the peer-review side, as well as production for all of the journals. Eventually, the IT and business analytics teams came under his wing as well. Kerry remained at PLOS, eventually overseeing nearly 80 staff, for five years.

In 2019, life had other plans once again, and Kerry stepped away from his successful role at PLOS for personal reasons. While evaluating future moves, fate intervened when Julie Steffen — AAS Chief Publishing Officer at the time and Kerry’s former coworker at University of Chicago Press — emailed to announce her retirement.

Now, as AAS’s Director of Scholarly Publishing, Kerry will lead and support the AAS publishing team and interface with IOP Publishing and eJournal Press, which provides the peer-review software. He’ll also maintain the various AAS publishing imprints as well as monograph publishing.

How Can We Make Your Experience More Delightful?

When you think about the process of publishing research in an academic journal, does the word delightful come to mind? Kerry hopes so, and one of his aims as Director of Scholarly Publishing is to make the publishing process delightfully effortless.

“One of the things that I’m really interested in is how we can change our interaction with our contributors to make it as frictionless as possible,” Kerry says. Part of this goal is ensuring that authors are only asked for materials that are absolutely necessary, rather than making them jump through hoops that take their time away from what really matters: research! (Kerry recalled a time when authors were asked to make print-ready CMYK versions of all their images — a task important for the publication of a physical article, but one that’s well outside a researcher’s purview.)

To succeed in this goal, Kerry welcomes feedback and constructive criticism from the tight-knit AAS community. “These journals are for the community in which we exist,” Kerry says. “I want to hear from our researchers how we can better perform for you. It’s not just about what we offer now, but what you would like to see in the future. I would love to hear if things go swimmingly, but I also do want to hear when things don’t go great. Constructive criticism is some of the most valuable feedback someone can ever give.”

Want to chat with Kerry about the AAS journals and share your feedback? You can find him at the AAS publishing booth throughout the upcoming 245th AAS meeting in National Harbor, Maryland.

logo of the American Astronomical Society

In 2017 we announced a new AAS-sponsored program for graduate students: the AAS Media Fellowship. This quarter-time opportunity is intended for current graduate students in the astronomical sciences who wish to cultivate their science-communication skills.

photograph of Lexi Gault

Lexi Gault (Indiana University) has been selected as the 2024–2025 AAS Media Fellow.

We are pleased to announce that Lexi Gault, an astronomy PhD candidate at Indiana University, has been selected as our AAS Media Fellow for 2024–2025.

Lexi majored in astronomy and mathematics at Valparaiso University, with minors in French and studio art. Now a fourth-year graduate student at Indiana University, Lexi works with Betsey Adams (ASTRON) and John Salzer to study the impacts of stellar feedback-driven outflows on the interstellar medium in nearby low-mass galaxies.

Outside of research, Lexi participates in a number of community outreach activities and serves as a research mentor. She’s also been to the top of the Green Bank Telescope a few times, most recently as a participant in the Green Bank Observatory Single Dish Summer School in 2023!

photograph of the 2023 Single Dish Summer School participants

Lexi (front row, just right of center) with the participants of the 2023 Single Dish Summer School. [Green Bank Observatory; CC BY-NC-ND 2.0]

As the AAS Media Fellow, Lexi will regularly write and publish summaries of the latest astronomy research on AAS Nova, assist in managing the distribution of press releases as part of the the AAS Press Office, and gain a broad understanding of the worlds of scientific publishing, communications, and policy. Lexi will also be assisting with the press conferences at the upcoming 245th meeting of the AAS, so please say hello if you’re attending the meeting in National Harbor, MD, next January!

As we welcome Lexi to the team, we’ll also soon bid farewell to Ben Cassese, our 2022–2024 AAS Media Fellow. Ben will be continuing his PhD studies at Columbia in the Cool Worlds Lab under David Kipping, where he is searching for moons around extrasolar planets. Following his enjoyable and enriching time as the Media Fellow, he hopes to pursue some freelance science writing and will be sure to say hi to the press team at future AAS meetings.

Please join us in welcoming Lexi as our new Media Fellow and wishing Ben the best in all his future endeavors!

multi-wavelength image of the Bullet Cluster

Editor’s Note: This week we’re at the 244th AAS meeting in Madison, WI, and online. Along with a team of authors from Astrobites, we will be writing updates on selected events at the meeting and posting each day. Follow along here or at astrobites.com for daily summaries, or follow @astrobites.bsky.social on Bluesky for more coverage. The usual posting schedule for AAS Nova will resume on June 17th.

Plenary Lecture: Scanning the X-ray Sky for Dark Matter, Kerstin Perez (Columbia University) (by Nathalie Korhonen Cuestas)

Throughout the universe, we’ve detected the indirect signatures of dark matter: a hypothetical form of matter that does not interact with normal matter through electromagnetism and makes up most of the matter in the universe. It’s seen in the rotation curves of galaxies, through gravitational lensing in the Bullet Cluster, and in the anisotropies of the cosmic microwave background. Dr. Kerstin Perez (Columbia University), the conference’s last plenary speaker, works to characterize the properties of dark matter through observations of X-ray photons, bringing us closer to understanding the matter that makes up so much of the universe.

It’s possible that dark matter particles interact through forces that we can’t currently understand using the standard model, producing photons with X-ray wavelengths. Perez leverages these interactions to look for “extra” photons as a signature of dark matter. However, it can be difficult to pinpoint which photons are coming from dark matter particles, and which photons are produced by normal, baryonic matter. Ideally, you’d observe a region with a high dark matter density and a low (or very well understood) background of photons from baryonic sources. Even though this technique can be tricky, Perez noted that even when a photon excess doesn’t end up being due to dark matter, it can still tell us something new about the background source.

To make her observations, Perez uses the NuSTAR instrument in a novel way. Normally, astronomers use photons that have traveled through the optics of the NuSTAR telescope, resulting in a small field of view. But one astronomer’s trash is another astronomer’s treasure; Perez uses photons that have come in from very large angles and hit the detector directly, rather than going through the optics system. This results in a larger pacman-shaped field of view, which can be cleverly aligned with a dark matter halo or a star, allowing Perez to search for photons produced by dark matter.

Dark matter particle theories come in lots of different flavors, and in her talk, Perez focused on two: sterile neutrinos and axions. Both types of particles only interact with gravity, and they could address other open questions in particle physics, not just that of dark matter. Perez showed observations of dark matter halos and Betelguese (a well-observed red supergiant) from NuSTAR, and while neither yielded a clear cut detection of dark matter, they do put strong constraints on the properties of dark matter. As these constraints get more stringent, we can get closer to either ruling out a theory or homing in on the true value. Perez ended by highlighting three proposed X-ray missions (HEX-P, GRAMS, and IAXO) that could apply this method with more precision, hopefully bringing us closer to understanding the nature of dark matter.

You can read Astrobites’s interview with Kerstin Perez here.

JWST image of the rho Ophiuchi molecular cloud complex and an illustration of the WL20 star system

Editor’s Note: This week we’re at the 244th AAS meeting in Madison, WI, and online. Along with a team of authors from Astrobites, we will be writing updates on selected events at the meeting and posting each day. Follow along here or at astrobites.com for daily summaries, or follow @astrobites.bsky.social on Bluesky for more coverage. The usual posting schedule for AAS Nova will resume on June 17th.

Table of Contents:


Helen B. Warner Prize Lecture: The Lives and Deaths of Star Clusters, and the Black Holes They Make Along the Way, Carl Rodriguez (University of North Carolina at Chapel Hill) (by Catherine Slaughter)

The Wednesday morning plenary lecture was given by this year’s Warner Prize recipient, Carl Rodriguez (UNC Chapel Hill). Rodriguez is a theoretical and computational astrophysicist, whose recent research focuses on the gravitational waves that could be produced by black holes in globular clusters. He opens the lecture emphasizing how our population of observed black holes has changed dramatically since 2015, when LIGO first came online. While gravitational waves have been used to observe a huge number of new black holes, Rodriguez highlighted a smaller set has been identified using radial velocity and (using Gaia) astrometry.

Rodriguez highlighted that newly identified populations often include black holes in the known upper mass gap; there are few black holes found with masses ranging from 65 to 135 times the mass of the Sun. The mass gap is a predicted result of late-stage stellar evolution, when stellar remnants of these masses are torn apart in highly energetic pulsational pair instability supernovae. We simply don’t expect to see isolated black holes of this size. Additionally, the observed astrometric binaries have masses and separations that are largely inconsistent with the expected parameters of common-envelope evolution of isolated binary stars. Rodriguez explained, however, that both of these oddities may be explained by the unique conditions inside globular clusters.

Rodriguez goes on to describe how black holes move throughout a globular cluster. Generally, dynamical friction causes very massive, dense objects to preferentially move toward the center of the cluster over relatively long timescales (~100 million years). Once they’re in generally the same space, black hole binaries can form through three-body system mechanics. In classical Newtonian mechanics, it is not possible for two unbound point particles to enter a bound orbit via standard gravitational interactions — there is simply too much energy in the system. It is possible, however, with the introduction of a third “interloper” star, which experiences a recoil effect, carrying the extra energy away with it. This phenomenon can explain the seemingly strange orbital parameters of the astrometric binaries. The remaining binary is either kicked from the cluster, merges while in the cluster, or gets disrupted by the cluster.

Of course, this all relies on a strong understanding of how globular clusters form in the first place. In order to better understand this, Rodriguez and his research group make use of their Great Balls of FIRE simulations. This project focuses on “daisy-chaining” three types of models. First, a high-resolution cosmological simulation shows how individual molecular clouds form in galaxies. Then, a cloud-collapse simulation takes in that output and models the creation of stars from the material. Finally, an N-body simulation shows how those stars interact and dynamically evolve over time. Their final result is a simulated galaxy, with mass similar to the Milky Way, containing a similar number of globular clusters to the Milky Way. These clusters are shown to have a similar age-alignment relationship to those in the Milky Way, and — most notably — a distribution of black hole masses that includes the upper mass gap. The question then becomes how the simulated mass-gap black holes formed. Rodriguez speaks primarily about two possible mechanisms: black hole mergers and progenitor star mergers.

An image of one of Rodriguez’s slides, outlining the structure of the Great Balls of FIRE simulation. [Slide by Carl Rodriguez]

Analysis of the simulation found that a given black hole is expected to experience, in the most extreme case, two or three mergers. This is because rapidly spinning black holes release gravitational waves in a preferred direction when they merge, causing the merger remnant to be “kicked” in the opposite direction. The more mergers a black hole experiences, the higher its spin, and the harder it gets kicked, eventually getting kicked from the cluster altogether. Indeed, they find only three of these most extreme hierarchical mergers manage to survive in the cluster. It is also possible that stars themselves merge over time, creating very massive objects that could, in turn, form significantly more massive stellar black holes. Using the simulation, Rodriguez and his research group find that because these clusters form hierarchically, they at some point have density profiles that are flat and relatively unstable, leading to runaway merger events.

An image of one of Rodriguez’s slides, showing the output of the Great Balls of FIRE simulation. [Slide by Carl Rodriguez]

Ultimately, Rodriguez explains, new populations of black holes look unlike how we expect because they were likely formed under fundamentally different conditions than we expect. His simulations show that black hole binaries are ten times more efficiently formed in cluster environments, compared to isolated environments. Importantly, recent observations of binary black holes in the upper mass gap can be well explained by the conditions in globular clusters.

You can read Astrobites’s interview with Carl Rodriguez here.

Return to Table of Contents.


Press Conference: More Stars and Distant Worlds (by Ben Cassese)

Wednesday morning, Madison, Wisconsin. As some clouds gathered over Lake Monona just outside the convention center, a comparatively friendly crowd of attendees of the 244th meeting of the AAS assembled to hear the final research-focused press briefing of the conference. Titled “More Stars and Distant Worlds,” this session had presentations split between individual interesting objects and looks towards future observations.

First up was Mary Barsony, who along with collaborators discovered an unusual and striking pair of young stars using the combined powers of ALMA and JWST. The researchers came upon this rare find after noticing something strange in archival images of a triple star system. Although two of the three members appeared about two million years old, measurements indicated that the third was somehow much younger. A closer look at this outlier revealed that what had previously appeared to be one strange star was actually a tightly bound pair, both of which are spewing out long jets of material. Intrigued, they observed the system again, this time using ALMA. This second look revealed nearly edge-on, skirt-like disks of gas around each star. This unique arrangement is an interesting laboratory to test theories of stellar formation and outflows, and a powerful demonstration of the benefits of combining multiple cutting-edge datasets. [Press release]

Next was Breanna Binder, California State Polytechnic University, Pomona, who jumped beyond the cutting-edge facilities of today and instead spoke about the work required to build the next generation of Great Observatories. The Habitable Worlds Observatory (HWO) currently exists only on paper, but by the 2040s, it should hopefully be a real, gigantic space telescope hard at work discovering and characterizing Earth-like planets. Before engineers and technicians can begin bolting together the observatory, however, astronomers need to figure out exactly where they want to aim the thing and what performance specs they need to achieve their ambitious goals. As part of that effort, Binder and collaborators went through a list of about 200 promising target stars to check which of these were amenable to hosting a habitable planet. They found that about a third of them had previously been observed by X-ray telescopes, and in many cases, these archival observations revealed a disappointing but important reality. Although many of their potential target stars appeared docile in the visible wavelengths, a good portion of them are furiously emitting X-rays that are strong enough to (likely) doom any chance of life emerging on the surfaces of their planets. Her presentation emphasized that while the road to HWO will be long, by the time the telescope reaches the launchpad, it’ll be powered on its journey to space both by not only its rocket but also by decades of planning. [Press release]

Next was Roman Gerasimov, University of Notre Dame, who quickly informed the audience that he is “Paid to figure out where the periodic table came from.” He goes about this substantial task by trying to find ancient brown dwarfs and measure their compositions. Brown dwarfs are too small to sustain nuclear fusion in their cores, which means that after being born bright and hot, they fade and cool over time. If one can find a collection of brown dwarfs that all should be around the same age, say a collection that lives in the same globular cluster, then measure their temperatures, the scientist could use them as “galactic chronometers” to estimate the age of the system. That’s exactly what Gerasimov and collaborators did: using images from JWST, they identified three ancient brown dwarfs in a globular cluster named NGC 6397. These puny, sub-Jupiter-sized worlds are likely among the oldest objects in our galaxy, and also likely are just the first of hundreds of similar discoveries. Gerasimov estimates that just one more set of JWST observations taken about three years from now would reveal hundreds more, since the longer baseline would allow the team to distinguish between members of the cluster and faint objects that happen to lie in front of or behind it.

Finally was Juliette Becker, University of Wisconsin-Madison, who described recent modeling of the “perilous” journey a planet with an ocean must embark on as its star grows old. This journey has elements of a good action movie: in order to reach a happy ending where the planet retains its ocean and travels on a stable orbit around its aging white dwarf, it must survive two distinct challenges. First, as its host expands from a typical main-sequence star into a red giant, the planet must avoid getting engulfed by the suddenly enormous central body (for those curious, when our own Sun becomes a red giant, Mercury and Venus will almost certainly fall prey to the ballooning star, though the jury is still out on whether Earth will similarly suffer). Should it successfully avoid getting eaten, then patiently wait out the star’s inevitable shrinkage from a red giant into a puny white dwarf, the planet will now find itself far too far away and cold for anything liquid to remain on its surface. In order to save its ocean, the planet must be kicked inwards towards the white dwarf by some other object in the system, then survive the resulting high-eccentricity migration and tidal dissipation required to land on a close-in, stable, warm orbit.

Becker has practical motivations for fleshing out the odds of each step in this string of hypotheticals, since planets around white dwarfs are significantly easier to characterize than planets around more generic solar-type stars. That’s because the primary technique astronomers use to measure the atmospheres of close-in planets, the transit technique, returns stronger signals as the radii of the star and planet become more similar. So, Becker and collaborators wanted to assess whether it would be worth our time to put the time into surveying these stars in the first place. Their conclusion? Although an ocean could technically survive the journey laid out above, “it’s not an easy process,” and it’s unlikely that a large portion of white dwarf planets have oceans.

You can view a video recording of this press conference or take a look at the presenters’ slides.

Return to Table of Contents.


Plenary Lecture: When Data is Not Enough: Illustrating Astrophysics for the Public, Robert Hurt (Caltech/IPAC) (by Will Golay)

Robert Hurt is a researcher at IPAC, an institution based at Caltech that supports four central data archives and 12 different NASA missions. Hurt is a self-described “AstroVizicist,” an expert in visualizing astronomical data for researchers and the public. In his talk, he aimed to motivate the importance of artistic visualization and its role in science communication.

Hurt shows one of the first pieces of acrylic artwork he made early on in his life, an image of a galaxy with several key features aiming to communicate how they are structured. However, Hurt points out that his galaxy painting from 1979 was missing a central bulge region. He noted that this was likely a product of the time: the images of galaxies at the time were being collected on photographic film plates, which would highly overexpose the galaxy’s central regions to have enough sensitivity to capture the lower surface brightness components near the edge. Hurt’s message is that scientific illustration is a sort of hypothesis representing our current understanding of the universe.

To determine if a scientific illustration is successful, we can ask if it is accurate, clear, and, most importantly, amazing. These three components — representing the science, communications, and art “Essential AstroViz Tensions” — can shape how we approach creating a new illustration. In any new science result, there are known facts, known falsehoods, and possibilities consistent with the data but not wholly affirmed. As a scientific illustrator, Hurt aims to capture the most important new known facts of the result, but he also mentions that we can’t possibly know everything. Sometimes, an illustrator must fill in the gaps left behind to paint a complete picture. They might even choose to specifically modify and include some “falsehoods,” such as synthetic colors or rescaling an object so it is visible in the image, to clarify the illustration (trading off accuracy for the value of communication).

Hurt then discusses several case studies of his work and how the scientific illustration process works. In one example, he shows an early image of the Milky Way that resulted in a few inaccuracies as new research emerged. So, he aimed to create a new, better illustration of what our own galaxy might look like to an external observer. Illustrating our galaxy in this way can provide insights that are otherwise challenging to understand with our “inside-out” view of the galaxy. This new image was informed by several scientific results, such as gas simulations, spiral arm models, observations along specific sightlines, and even some unpublished results. The new image ended up being so well-constructed that a feature on the far side of the galaxy, the Scutum-Centaurus Arm of the Milky Way, was so accurate that a different researcher ended up confirming some key details and contacted Hurt because he was concerned he had access to his unpublished data! The artist had simply used some basic symmetries.

The updated illustration of the galaxy incorporates updates to the original image informed by accurate science results. This image is our best guess of the Milky Way's structure.

The updated illustration of the galaxy incorporates updates to the original image informed by accurate science results. This image is our best guess of the Milky Way’s structure. [Slide by Robert Hurt]

Hurt concludes by highlighting his non-traditional career path and the importance of fostering non-traditional and traditional academic career skills in our students. He states that we never know where a student will end up and how their skills outside of the classroom may contribute to a new, unique future role in astronomy that we can’t even predict. It is important for mentors to foster both of these skillsets in their students, even though that might mean a student is working on something beyond their research. Hurt’s illustrations are available online and are free to share with anyone.

You can read Astrobites’s interview with Robert Hurt here.

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Press Conference: Citizen Science from the 2023/2024 Solar Eclipses (by Catherine Slaughter)

Wednesday afternoon brought with it a press conference highlighting citizen science from the 2023 (annular) and 2024 (total) eclipses. Speaking at the conference were Amir Caspi (Southwest Research institute), Angela Des Jardins (Montana State University), Dawn Davies (Hill Country Alliance) and Kate Russo (Being in the Shadow).

A slide from Caspi's press release. It shows a composite image of the solar corona taken by his citizen science teams. The colors indicate the angle of polarization. Caspi's zoom image can be seen on the right.

Composite image of the solar corona taken by his citizen science teams. The colors indicate the angle of polarization. [Slide by Amir Caspi, photo by Catherine Slaughter]

First up was Amir Caspi, reporting on the results of the Citizen CATE project. Citizen CATE featured an observing network of community participants and aimed to study polarization in the solar corona. He highlights that total eclipses provide better ground-based coronal observing than a coronagraph does because eclipses also create pseudo-dark-sky conditions. Because the coronal activity the team was searching for lasts longer than the few minutes an eclipse can be observed at a single site, the Citizen CATE team gave identical, specialized telescopes to 35 teams along the eclipse path. He highlights that the communities that participated were all allowed to keep the equipment for future science and outreach purposes. In all, more than 85% of the sites were able to obtain full or partial eclipse data for the project.

Next up to the podium was Angela Des Jardins, speaking about her eclipse ballooning project, which aimed to measure the atmospheric response to the eclipse leading up to and after totality. Stratospheric ballooning is a multi-disciplinary endeavor, and is useful because it creates space-like conditions without the need for a rocket. For the eclipse project, two teams of researchers — an atmospheric science team and an engineering team — spent the 24 hours preceding the eclipse and 6 hours proceeding, launching stratospheric weather balloons with weather sensors, accelerometers, cameras, and other student-designed experiments. Her primary goal was to observe atmospheric gravity waves (which, she highlights, are not the same as gravitational waves). The experiment was successful, with the first confirmed observations of eclipse-driven gravity waves. [Press release]

Then Dawn Davies stepped up to speak about her project, LightSound. LightSound is a solar eclipse sonification device, made for those in the blind and low-vision community to better experience eclipses. Leading up to the 2023 and 2024 eclipses, LightSound received more than 2,400 requests for devices internationally. Over the course of eight workshops, 420+ volunteers of a broad range of ages and previous building experience created more than 900 devices for libraries, museums, community task forces, blind and low vision services, national parks, senior centers, and more. The team also set up a live-streamed webinar in conjunction with the American Council for the Blind, which reached an audience of more than 2,500 people. As of now, the LightSound team is looking ahead to the 2026 and 2027 eclipses, and are hoping to implement a haptic feedback feature to the device. [Press release (PDF)]

Finally, Kate Russo took the stage to describe her project, Being in the Shadow. A clinical psychologist by trade and eclipse chaser by hobby, Russo and her collaborators work to observe the feeling of awe inspired by viewing a solar eclipse through brain wave signatures. She defines awe by two specific experiences. The first is vastness, an understanding of something greater than ourselves, and the second is accommodation, the way we re-align our perspectives accordingly.  In previous phenomenological research, Russo identifies six experiences that people most often report experiencing during a total eclipse: a sense of wrongness, a primal fear, awe, connected insignificance, euphoria, and a desire to repeat (yielding the appropriately themed acronym “SPACED”). In a pilot project conducted during the 2023 annular eclipse, their primary goal was to simply test the efficacy of the brain-wave mapping technology. What Russo found, however, was that even in a non-total eclipse, they were able to observe awe in every single participant’s data. Looking forward, they are hoping to repeat the experience at the 2028 eclipse in Australia (where Russo primarily works), and possibly extend the project to other astronomical events. [Press release (PDF)]

An image of the panel at the eclipse outreach press conference

An image of the panel at the eclipse outreach press conference. Shown (left to right) are Susanna Kohler (at the podium), Angela De Jardins, Dawn Davies, and Kate Russo. Amir Caspi presented from zoom and is not shown. [Photo by Catherine Slaughter]

You can view a video recording of this press conference or take a look at the presenters’ slides.

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Royal Astronomical Society Gold Plenary Lecture: Challenges to the Cosmological Model, John Peacock (University of Edinburgh) (by Nathalie Korhonen Cuestas)

Over the course of 67 years, modern cosmology was born and matured into the current standard model, known as Λ cold dark matter (ΛCDM). In his plenary lecture, Dr. John Peacock laid out the history of cosmology, highlighting the measurements that got us to where we are now, explained some of the possible problems with ΛCDM, and outlined how recent results address these challenges.

There’s a plethora of evidence supporting ΛCDM. From redshift measurements of Type Ia supernovae, to the large-scale structure of the universe, to the anisotropies of the cosmic microwave background (CMB), many signs point towards ΛCDM. However, there are some areas of the model that we don’t fully understand — including but not limited to the nature of dark energy and dark matter — and some areas of the model that appear to be in conflict with observations. Peacock touched on four major sources of tension — large-scale streaming velocities, the CMB dipole, Hubble tension, and lensing of the CMB — and focused primarily on the last two.

You may know that the universe is expanding at an ever increasing rate, and the Hubble constant describes the speed of this expansion. There are a number of different ways you can estimate the Hubble constant, but they generally fall into two categories. One method involves measuring the distance to and velocity of distant galaxies. These two quantities are linearly related and the slope of the line can give you the Hubble constant. Alternatively, you can calculate the Hubble constant from the temperature of the CMB, which is very precisely measured. But there’s a problem: these two methods yield different values for the Hubble constant. Typically, Type Ia supernovae or Cepheid variable stars are used to calculate the distance measurements, but, Peacock said, these methods might be introducing unknown systematic uncertainties. He also showed that when a different standard candle (J-region asymptotic giant branch stars in this case), you can get a value for the Hubble constant that more closely agrees with the CMB value.

The second source of tension Peacock discussed was the results from weak gravitational lensing studies. Mass warps spacetime, and this leads to a lensing effect that produces distorted images. If you know what the undistorted image should look like, you can use the distortions to calculate the mass that must have been along the line of sight and produced the lensing. The technique can be applied to the CMB; by measuring distortions in the CMB, you can back out the amount of mass that must have been along the line of sight. Since the CMB is the edge of the visible universe, the mass along the line of sight probes the distribution of mass throughout the universe, which is fundamentally determined by cosmology.

Peacock showed that we do in fact observe slight distortions to the CMB, and the overall distortion is in good agreement with ΛCDM. However, when distortion was broken down into different redshift intervals, astronomers found something different. When only considering the mass at high redshift, the results were consistent with ΛCDM, but this was not the case at lower redshifts, in the local universe. The result might point towards a potential time evolution in ΛCDM, specifically in the dark energy component of the model (that’s the Λ). However, Peacock was careful to emphasize that these results are still in their early stages, and further study is needed before we make any major adjustments to our cosmological models.

You can read Astrobites’s interview with John Peacock here.

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Solar Physics Division Harvey Prize Plenary Lecture: Dissipation and Excitation: The Role of Kinetic-Scale Waves and Instabilities in the Evolution of the Solar Wind, Kristopher G. Klein (University of Arizona)

The Karen Harvey Prize is awarded by the Solar Physics Division of the AAS in recognition of significant contributions to solar physics early in one’s career. This year, the award went to Kristopher Klein of the University of Arizona. Klein studies the solar wind — the tenuous plasma that constantly streams out from the Sun and fills the solar system. Because the Sun is by far the closest star to Earth, there are types of data that we can collect from the Sun that we simply can’t get for any other star or distant plasma environment. While Klein jokingly laments that many solar physicists interact not with pretty pictures of the Sun but instead with densely packed plots of particles and electric and magnetic fields, studies of the Sun have far-reaching implications.

Klein’s work uses simulations to understand how energy is transferred within the solar wind plasma. Energy can be transmitted by waves, instabilities, and turbulence, which transfers energy from large spatial scales to small spatial scales. Studying these factors can help researchers understand electron and proton heating, which can in turn help to interpret observations of distant plasma environments, such as the pictures of Sagittarius A*, the supermassive black hole at the center of the Milky Way.

In addition to simulations, solar physicists work with an abundance of spacecraft data: there are currently 20 missions (27 spacecraft in total) capable of making in situ measurements of the solar wind, and 14 more missions are currently being formulated or implemented. Using this fleet of spacecraft, researchers can extract the basic properties of the solar wind and derive more complex parameters, like the plasma beta (the ratio of the thermal pressure of a plasma to its magnetic pressure). Because the plasma beta varies greatly with position in the solar system, different locations within the solar wind can be used as analogs for many different plasma environments across the universe.

Klein expanded on the projects that he and his research team have undertaken to track down the ways in which energy flows within the solar wind. While important advances have been made with existing data and simulations, most current spacecraft missions measure the properties of the solar wind at a single point, taking measurements as the solar wind blows across the spacecraft. (A few missions like the Magnetospheric Multiscale mission involve multiple spacecraft working in tandem.) Klein introduced the upcoming HelioSwarm mission, which will be composed of nine spacecraft that explore the solar wind, magnetosheath, and foreshock on a variety of spatial scales to study these regions in an entirely new way. With new views of the solar wind incoming, we can expect our knowledge of the solar wind and other plasma environments across the universe to increase in leaps and bounds!

image summarizing current heliophysics missions

A summary of the current (as of 2022) fleet of heliophysics missions. [NASA’s Goddard Space Flight Center]

You can read Astrobites’s interview with Kristopher Klein here.

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ten spiral galaxies imaged by JWST

Editor’s Note: This week we’re at the 244th AAS meeting in Madison, WI, and online. Along with a team of authors from Astrobites, we will be writing updates on selected events at the meeting and posting each day. Follow along here or at astrobites.com for daily summaries, or follow @astrobites.bsky.social on Bluesky for more coverage. The usual posting schedule for AAS Nova will resume on June 17th.

Table of Contents:


Plenary Lecture: Dark and Quiet Skies for the Future of Astronomy and of the Space Environment, Aparna Venkatesan & Teznie Pugh (University of San Francisco and McDonald Observatory, UT Austin) (by Will Golay)

Aparna Venkatesan (University of San Francisco) and Teznie Pugh (McDonald Observatory, UT Austin) started the second day of the AAS by discussing the exponentially growing challenges of protecting dark and quiet skies. Venkatesan and Pugh are co-chairs of COMPASSE (Committee for the Protection of Astronomy and the Space Environment), an AAS committee dedicated to preserving the viability of ground-based, orbital, and lunar astronomy.

There are growing threats to astronomy across the electromagnetic spectrum, the most well known being light pollution. A recent paper used citizen science reports of star visibility and found that the reduced number of visible stars can be explained by the sky brightness increasing between 7% and 10% every year for the last 11 years. If this trend continues, the number of visible stars in the night sky will halve every 10 years, an existential threat to ground-based optical astronomy. The impact on major astronomical observatories is also profound. Another recent result showed that about two-thirds of major astronomical observatories have sky brightnesses exceeding the International Astronomical Union’s recommended 10% above natural levels.

However, the threat does not end in the optical or on the ground. Radio-frequency interference is another rapidly growing problem that could wipe out ground-based radio observatories. At the other end of the spectrum, space-based nuclear power could threaten space-based high-energy observatories like Chandra (#SaveChandra). Also in space, the growing number of satellites has posed a major problem for ground-based observation. Eighty percent of all active satellites have been launched in the last four years, and 60% of active satellites are part of the Starlink constellation. As of 29 May 2024, there are 547,267 combined International Telecommunications Union (ITU) & Federal Communications Commission (FCC) applications for new frequency allocations for space-based satellites. The impact of these satellites is manyfold: from increasing the sky brightness, streaking in images, and the impact of launches (which are not yet well known), 500,000 satellites would make ground-based astronomy almost impossible. Given current predictions on satellite launchers, the Vera Rubin Observatory anticipates streaking in 30% of images during twilight hours.

A zoom-in of the radio frequency allocation plot showing the location of the 21-cm line relative to the frequency allocations

A zoom-in of the radio frequency allocation plot showing the location of the 21-cm line relative to the frequency allocations. The 21-cm line is not a frequency protected for astronomy. [Slide by Aparna Venkatesan and Teznie Pugh]

The impact of brighter skies extends far beyond professional astronomers. Amateur astronomers will also suffer the same effects, and the implications on animal and bird migration patterns are just starting to be understood. Some Indigenous populations, which have already disproportionately been impacted and repeatedly displaced, rely on wayfinding with constellations and asterisms. The rising sky brightness already has measurable impacts on this navigation method by reducing the number of visible stars.

However, all is not lost! COMPASSE is taking many steps to combat these challenges. COMPASSE provides templates for local ordinances and advocates for dark skies, education, and outreach in local communities. The committee also works with government organizations like the FCC, the Federal Aviation Administration, the US State Department, etc., to provide comments on the impact of new policies on dark and quiet skies. They are increasing awareness by publishing in scientific journals and popular media outlets, and they’ve taken many more steps to begin combating this issue. Venkatesan and Pugh highlighted that the story is not complete yet, and that it is our story to write by getting involved in advocacy for dark and quiet skies.

You can read Astrobites’s interview with Venkatesan and Pugh here.

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Press Conference: From the Galactic Center to the Galactic Disk (by Nathalie Korhonen Cuestas)

The first press conference of the day included five different speakers who described their work on Sagittarius A* (Sgr A*) — the supermassive black hole (SMBH) at the center of our galaxy — and its surroundings. Sgr A* gives us a rare chance to study inactive black holes, which are otherwise too faint to observe with much detail.

The first speaker, Grace Sanger-Johnson (Michigan State University), presented X-ray observations of Sgr A*, which were taken over a period of eight years by the NuSTAR telescope. A puzzling characteristic of Sgr A* is that it flares in X-ray wavelengths. Over a period of a couple hours, Sgr A* can become up to 600 times brighter than it normally appears. The origin of these cosmic fireworks is currently unknown, but there are two main hypotheses: the flares could originate from the magnetic fields in plasma very close to the black hole, or they could be the result of a star coming too close to the black hole and losing some of its mass. Sanger-Johnson’s observations show that there is a correlation between the brightness of a flare and the hardness of a flare. Here, “hardness” refers to how much of the light emitted is at shorter, more energetic wavelengths. A harder flare has more energy at shorter wavelengths, and Sanger-Johnson found that harder flares were generally brighter. This correlation could point to two different origins for these X-ray flares: one that produces dimmer, softer flares, and another that produces brighter, harder flares. Further observations of Sgr A*’s flares will help astronomers determine if this is indeed the case. [Press release]

Next up was Jack Uteg, a rising sophomore at Michigan State University. His talk shifted focus from Sgr A* to the ring of molecular gas that resides around 100 parsecs from the galactic center. This gas, known as the central molecular zone (CMZ), can be observed in X-ray, but we know that molecular gas cannot emit at this wavelength by itself. Therefore, these X-rays may have originated from Sgr A*, and are now being reflected by the CMZ. Uteg specifically studies the emission from a region known as the Bridge Cloud. The distance between Sgr A* and the Bridge Cloud means that light takes about 200 years to travel from Sgr A* to the Bridge Cloud, where it can be reflected. This means that any observations of the Bridge Cloud tell us what Sgr A* was up to 200 years ago. Using X-ray observations taken over 24 years, Uteg reconstructed the X-ray emitting history of Sgr A* and found that around 200 years ago, Sgr A* underwent an outburst that made it 100,000 times brighter than it normally is! [Press release]

Continuing with the theme of the CMZ, Dylan Paré (Villanova University) discussed his observations of the magnetic fields in the CMZ. The FIREPLACE (Far-Infrared Polarimetric Large-Area CMZ Exploration) survey used the polarization of light from the CMZ to map the magnetic fields that thread the clouds. Paré found that the magnetic field was preferentially oriented in two directions, and that higher density regions such as The Brick (see the first inset panel in the image below) have more well-aligned magnetic fields. In the galactic disc, the opposite is observed to be true — denser clouds are less likely to have well-aligned magnetic fields. While further analysis of the different regions of the CMZ is needed, it’s possible that the observed magnetic fields are the result of a large-scale magnetic field, running perpendicular to the galactic plane, being sheared by the molecular clouds.

This image shows the structure and magnetic fields of the CMZ. Cloud-like structures are shown in purple and cyan, and thin yellow streaks can be see crossing the clouds vertically. The direction of the magnetic field is also shown using short white lines which are aligned with the field direction. There are three inset panels which show zoom-ins of three regions: The Brick, the 20 km/s cloud, and Sgr C. In these insets, the magnetic field lines are well-ordered and appear to align with the cloud.

This picture shows you the CMZ, and the inset panels zoom in to the larger image. Radio emission is shown in yellow, emission from warm dust is shown in purple, and emission from cool dust is shown in cyan. The direction of the magnetic field is shown by the white lines. [Paré et al. 2024]

Another region observed by the FIREPLACE survey is Sagittarius C (Sgr C), an intriguing region with unusually high star formation. Jianhan (Roy) Zhao (UCLA) described the various components of Sgr C and how we can use them to learn more about the mechanisms at play in the CMZ. In the image you can see bright yellow streaks, which are radio filaments. One of these filaments originates in Sgr C, appearing to emanate from a shell of ionized gas that surrounds a molecular, star-forming cloud. One possible source of radio filaments is magnetic reconnection, a high-energy phenomenon that can accelerate electrons and cause them to emit in the radio wavelengths. In Sgr C, Zhao found that the magnetic field lines are converging towards the radio filament, supporting the idea that magnetic reconnection is powering the radio emission. The fact that the radio filament is seen to originate in an ionized region further supports this idea, since in order for electrons to be accelerated, they have to be free.

Last but not least was Dr. Anthony Minter (Green Bank Observatory), who discussed his search for dust and molecules in Smith’s high-velocity cloud. High-velocity clouds are clouds that are flying towards the Milky Way, potentially providing the fuel needed to sustain star formation. Clouds in the Milky Way contain different molecules and dust grains, but Smith’s high-velocity cloud was observed to contain no dust or molecules. It could be that the cloud originally did contain dust and molecules, but over time, they became dissociated, or, it could be that the cloud was formed from a pristine environment. In the galactic disc, we know that clouds further from the galactic plane have less dust and molecules. Minter found that clouds near the galactic center have a similar, but steeper gradient. This means that a cloud at the galactic center will have fewer molecules and dust grains than a cloud at a similar height from the galactic plane, but over the galactic disc. These kinds of abundance patterns help us to understand the structure of the Milky Way and potentially help reconstruct the events that determined the evolution of our galaxy. [Press release]

You can view a video recording of this press conference or take a look at the presenters’ slides.

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Unlocking the Mysteries of Exoplanets: The Crucial Role of Laboratory Research, Erika Kohler (NASA Goddard Space Flight Center) (by Catherine Slaughter)

This summer’s AAS meeting is a joint session with the Laboratory Astrophysics Division (LAD). As part of this joint meeting, Dr. Erika Kohler (NASA Goddard Space Flight Center) gave Tuesday’s midday plenary lecture. In this talk, Kohler promoted the use of lab-based experiments in astrophysical research and highlighted a number of her group’s projects, including the prep work for the forthcoming Deep Atmosphere Venus Investigation of Noble gases, Chemistry, and Imaging (DAVINCI) mission.

The talk starts out posing a question that motivates much of the work we do as scientists: “We found it, why not study it?” Kohler describes how recent technological innovation has allowed us to develop advanced spacefaring probes and respond to this question using in situ measurements of solar system planets. The catch, she notes, is that even the most advanced tech could not make in situ measurements of exoplanets. From this, Kohler outlines her talk’s key takeaways: that lab research is fundamental and complements all other astrophysics work, and that (given the cross-disciplinary nature of exoplanet research) communication pathways and user engagement propel us forward. To underscore these ideas she gives two examples from her own research.

The first comes from a study of cloud formation in exoplanet atmospheres. Solar system planets, Kohler explains, represent a very limited region of possible exoplanet parameters, especially in terms of atmospheric pressure and temperature. “If you’re only designing experiments to describe [the solar system planets],” she says, “you’re missing a whole universe out there.” In the project, Kohler and her team used lab-based experiments to recreate the very extreme atmospheric environments found on distant exoplanets. Their goal was to experimentally determine saturation vapor pressure curves — mathematical descriptions of the pressures and temperatures at which a given material will form clouds — for a number of known and expected molecules in exoplanet atmospheres. The preexisting curves were created using calculations based on Earth-like conditions. They found that the heights at which clouds form in a given atmosphere are different in extreme environments, which changes our interpretation of possible exoplanet atmosphere observations. This is a result that could only be reasonably obtained in a lab setting.

A slide from Kohler's talk, showing the Orbital Distance-Mass parameter space scatter plot for identified exoplanets at present. The plot is lined in white with white text on a black background, and the data points are colored according to discovery method (solar system planets, transit, radial velocity, microlensing, and imaging). The sections of parameter space spanned by the solar system planets is highlihgted in purple.

A slide from Kohler’s talk, showing the orbital distance–mass parameter space scatter plot for identified exoplanets at present. [Slide by Erika Kohler]

The second example is a study conducted in preparation for the launch of DAVINCI. The mission will include a probe that descends down to the surface of Venus, taking images of the surface in near-infrared and making atmospheric measurements along the way. In order to obtain usable images, however, it is important to ensure that the atmosphere of Venus is reasonably transparent to infrared light. Kohler’s group began by studying the changing opacity of CO2 in the varying temperatures and pressures of Venus’s atmosphere. They conducted a simulated descent, taking observations of infrared transmission through CO2 at conditions mimicking the atmosphere from 55 to 7 km above the surface. In doing so, they are able to identify the wavelengths at which the atmosphere can be expected to become opaque at some point in the probe’s journey. Along with being foundational work for the future DAVINCI mission, these experimental results have huge implications for JWST, which observes in the mid-infrared, highlighting the necessity of lab work as a supplement to distant observation.

A slide from Kohler's talk showing a sprawling graph-map diagram of the many features studied in exoplanet research. They are spacially organized into broad groups labled "Stellar Effects," "Planetary Systems," and "Planetary Properties." Each feature is colored according to whether it is directly observable, modeled in a way that is constrained by observations, or accessible through direct modeling only.

A slide from Kohler’s talk showing a sprawling graph-map diagram of the many features studied in exoplanet research. [Slide by Erika Kohler]

Kohler finishes the talk encouraging the crowd to pursue three actionable challenges: 1. Talk to people in other subfields. 2. Look at the assumptions in our own research, and see if they’ve ever been verified in the lab. 3. Take a multi-method approach to research, combining lab-based, modeling, and observational techniques. She leaves us with a reminder that lab-based research allows us to both describe and predict astrophysical observations, and that we want to be prepared before first light. 

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Press Conference: Massive Black Holes and Surprising Spirals (by Kerry Hensley)

Fan Zou (Penn State University) opened the afternoon press conference with a discussion of supermassive black hole growth. Despite nearly all massive galaxies having supermassive black holes, it’s still not known exactly how these objects get so massive. Accretion and mergers are the two possible growth mechanisms, and researchers need to understand both processes to reconstruct the growth history of black holes. Zou explained that astronomers study black hole accretion through X-ray observations, and they study mergers through supercomputer simulations. Combining results from Chandra X-ray Observatory, eROSITA, and XMM-Newton — three premier X-ray observatories — with output from the IllustrisTNG simulations, Zou’s team found that accretion played a larger role in black hole growth than mergers did under most circumstances. The growth rate due to both mechanisms was higher in the early universe, although the two mechanisms have declined at different speeds. Today, mergers play a larger role relative to accretion than in the early universe. [Press release]

illustration of a quasar with outflowing winds

Illustration of a quasar with outflowing winds. The spectra at the top right shows how the absorption line has shifted to bluer wavelengths over time. [NASA/CXC/M. Weiss, Catherine Grier and the SDSS collaboration]

Robert Wheatley and Catherine Grier (University of Wisconsin-Madison) reported on their study of a quasar: a supermassive black hole with a hot, luminous accretion disk that emits radiation across most of the electromagnetic spectrum. Quasars often have powerful winds or outflows that travel at millions of miles per hour out from the accretion disk. Because these winds can block the light from the hot accretion disk, they are visible in quasar spectra as absorption lines. Using observations from the Sloan Digital Sky Survey Black Hole Mapper Reverberation Mapping Project, Wheatley, Grier, and collaborators demonstrated that the outflows from the quasar SBS 1408+544 (also called SDSS-RM 613) have been accelerating over the past eight years because of radiation pressure from the luminous accretion disk. This acceleration was evident from the blueward shift of an absorption line of carbon. While previous observations have hinted at accelerating quasar outflows in a handful of spectra, this new work uses 130 spectra, providing an unprecedented new look at this phenomenon. [Press release]

Next, Riccardo Arcodia (MIT) presented a study on massive — not supermassive! — black holes in low-mass galaxies. Studying these somewhat-less-than-supermassive black holes in the nearby universe can help researchers understand how supermassive black holes grew from lower-mass seeds in the early universe. Accreting black holes emit light across the electromagnetic spectrum and can be highly variable, so Arcodia’s team searched for low-mass galaxies that are variable in the optical and infrared to identify candidate massive black holes. Of the 200 candidate massive black holes, only 17 emitted X-rays. This result is unexpected because accreting supermassive black holes are extremely luminous in X-rays, and the team estimated that X-rays from the black holes in their sample should have been detectable. This might mean that lower-mass black holes have a different accretion mode compared to supermassive black holes, possibly because of the lower gravity, clumpier interstellar medium, or other factors. [Press release]

Lastly, Vicki Kuhn (University of Missouri Columbia) presented some new results from JWST on spiral galaxies. Previous studies using the Hubble Space Telescope have found that there are very few spiral galaxies earlier than a redshift of z = 2, which corresponds to when the universe was just a few billion years old. Kuhn’s team identified 873 galaxies with high stellar mass and redshifts between 0.5 and 4 in observations from JWST, which can look farther back in time than Hubble can. A team of six researchers visually classified each galaxy in the sample as spiral or not, and they found that JWST sees more spirals than Hubble did, especially at low redshift. To account for the fact that spiral structure is harder to discern at high redshift, Kuhn’s team created a sample of mock high-redshift galaxies. After determining how redshift affects the fraction of galaxies in which spiral structure is visible, the team found that about 30% of galaxies are spirals out to a redshift of z = 3. This is far more spirals than found in previous studies, suggesting a need to recalibrate our expectations for when and how spiral structure formed in early galaxies. [Press release]

You can view a video recording of this press conference or take a look at the presenters’ slides.

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Plenary Lecture: Leveraging AI to Transform the Astronomy Data Revolution into a Discovery Revolution, Cecilia Garraffo (Center for Astrophysics | Harvard & Smithsonian) (by Will Golay)

Cecilia Garraffo is a researcher at the Center for Astrophysics | Harvard & Smithsonian and the director of AstroAI. She is an expert in machine learning (ML) and artificial intelligence (AI) data analysis methods. She has developed novel techniques for using machine learning to uncover unique and exciting results from large astrophysical datasets. In her talk, she aimed to highlight what AI can contribute to research in astrophysics.

Garraffo motivated the need for AI methods by reminding us of an important point: although we are building massive observatories that will be coming online in the next five to ten years, are we, as a community, prepared for the immense data influx that will ensue? Once observatories like the Vera Rubin Observatory and the Square Kilometre Array begin observing, we will generate more data in one year than all currently existing astrophysical data. We are entering the era of petabyte astrophysics, an era we are not yet prepared to begin. The data volumes are not the only consideration: as astrophysics research becomes increasingly multi-wavelength and multi-messenger, causing datasets to become heterogeneous, it is even more critical that we have methods that can unify the picture and maximize the scientific value of such unique datasets.

AI is one tool we can apply to begin preparing for the upcoming massive influx of data. Garraffo argues that AI has the unique ability to search for patterns and classes intentionally (even if we don’t know what those patterns are a priori), enabling a chance for discovery spaces that would otherwise be inaccessible in smaller datasets. Even the most basic dimensionality reduction and clustering methods have successfully identified new anomalies in large datasets that we can later follow up on.

How exactly do we execute such a search using ML methods? The astronomy community needs experts in AI to help develop strategies specific to our kind of data. Astronomical data often differs from the data used to train large language models (LLMs) in several ways. Our data are biased and complex, could be multimodal, almost always incomplete, and undoubtedly sparse. To address these issues, we need to take specific steps to prepare our data and our ML models, which require user expertise in identifying methods and successfully applying them in the context of astrophysical research.

Garraffo then shared several examples of how AI has been used in various research contexts inside the AstroAI collaboration. One particularly striking example she shared was using ML methods to generate new “realistic” images of a black hole accreting material for comparison with images from the Event Horizon Telescope (EHT). Since general relativistic magnetohydrodynamic simulations are costly to run, we can use ML methods to interpolate between the model’s parameters. In the case of EHT, they are interested in using these methods to generate images of a black hole with differing spins, significantly affecting how the accretion will appear in EHT images.

A slide from Cecilia Garraffo's presentation showing two images of a black hole that were generated by simulation and one image that was generated from ML methods. Garraffo is illustrating that the human eye is not well-suited to distinguish between these cases.

A slide from Cecilia Garraffo’s presentation showing two images of a black hole that were generated by simulation and one image that was generated from ML methods. Garraffo is illustrating that the human eye is not well suited to distinguish between these cases. [Photograph by Will Golay]

Although ML astrophysics methods are just starting, Garraffo is excited to continue sharing them and educating the community via the AstroAI collaboration. The collaboration aims to educate students about how AI methods can be used in astrophysics research and begin developing a new era in which these methods are common throughout a wide variety of subfields. Stay tuned for more updates about the AstroAI collaboration at the Center for Astrophysics on their website!

You can read Astrobites’s interview with Cecilia Garraffo here.

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Plenary Lecture: With a Wild Surmise: A New Era of Exoplanet Exploration, Tom Beatty (University of Wisconsin at Madison) (by Jessie Thwaites)

Wrapping up today’s talks was Dr. Tom Beatty, whose plenary lecture explored exoplanets, specifically how we can classify them. We already know of more than 5,600 exoplanets, and that number just keeps growing! He discussed how we can measure a planet’s atmosphere to learn how exoplanets form, explore what makes a planet habitable, and search for signatures of water and oxygen that would be necessary to support life.

The attempt to classify exoplanets is multifaceted, he says, including searching for trends in their mass, gravity, age, metallicity, clouds, specific elemental abundances, and more. But these quantities have complicated relationships; for example, he discusses how ambiguity in cloud models on the planet’s surface can change the abundance measurement we get. These measurements of the spectra of these planets are made via transmission (seeing the spectral lines that appear when the planet passes in front of its star) and emission (seeing the spectral lines than disappear when the planet passes behind its star).

Central to the themes of his talk were how improvements in technology have made these detailed and accurate measurements possible. Initially, these measurements were done with the Spitzer Space Telescope, and massively improved upon with the Wide Field Camera 3 instrument on the Hubble Space Telescope, which allowed for more precise and spectroscopic measurements. And now, with JWST’s improved sensitivity, we can measure carbon and oxygen molecules in exoplanet atmospheres for the first time, get spectroscopic measurements of clouds, and even search for signatures of life on exoplanets!

slide describing what we could learn using JWST observations in the near future, and a graphic with properties of exoplanets that should be included in their classifications, including age, gravity, clouds, mass, irradiation, bulk metalicity, and mixing.

New questions about our understanding of exoplanets, and properties of exoplanets that are currently being studied. [Slide by Tom Beatty]

But searching for biosignatures requires more than just understanding the atmosphere on these planets, he says, so researchers have formed the Wisconsin Center for Origins Research (WiCOR) to bring together astronomy, chemistry, integrative biology, geoscience, bacteriology, botany, and atmospheric and oceanic studies to search for life on exoplanets in a multidisciplinary way.

You can read Astrobites’s interview with Tom Beatty here.

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