Open research questions in Astro and Planetary Science
35 unresolved questions extracted from the limitations and future-work sections of 501 Astro and Planetary Science papers in our library. Each links back to the study that raised it.
What the literature leaves open
Only KELT-20 b clearly prefers the presence of OH features, but the OH abundance constraints are limited by the low opacity of this species in the K band. Our efforts to constrain C/O ratios were limited by the impact of thermal dissociation and the sensitivity of the C/O ratio inference to the exact vertical mixing treatment.
Atmospheric Characterization of Six Ultrahot Jupiters from <i>K</i> -band High-resolution Spectroscopy · 2026 · DOIThe Uranian moons Ariel, Umbriel, Titania, and Oberon are enriched in CO2 mixed with CO, but the origin(s) of these carbon oxides, be they primarily native or radiolytic, remains uncertain.
Tracing the source of carbon oxides on the large moons of Uranus · 2026This decoupling emerges directly from the simulation data, showing that a single characteristic impact velocity is insufficient to represent the full dynamical interactions. The results from all three figures establish that mean velocities are insufficient to characterize dust–planet interactions. Together, these findings demonstrate that mean impact velocities are insufficient to characterize dust–planet interactions; the full velocity distribution must be considered when assessing impact-driven surface modification, exosphere generation, and volatile delivery across the terrestrial planets.
Modeling and Analysis of Main-belt Asteroidal Dust Flux and Velocity Distribution at Inner Planets · 2026 · DOIOur derived photometric parameters reproduce established correlations from both targeted studies and surveys using sparse data: strong G1 − G2 anti-correlation, albedo dependencies, and clear taxonomic separation in the G1, G2 parameter space.
Through this work we have presented new physical and astro- metric constraints derived from stellar occultations for 101 target asteroid systems observed between October 2023 and February 2026. This study represents the first dedicated effort targeting intermediate-size objects in the 5–100 km range through a co- ordinated occultation strategy, rather than isolated single-object campaigns. In particular, the occultation of (5044) Shestaka on October 23, 2024, gathered an unprecedented number of partic- 100101102103Diameter (km)05101520253035404550Total number of chordsArchived Occultations database (Herald+2020)GaiaMoons Occultations (this work)(5044) Shestaka(1127) Mimi(35420) 1998AG6(36882) 2000SW155 A&A proofs: manuscript no. output via anonymous ftp to cdsarc.u-strasbg.fr (130.79.128.5) or via http://cdsweb.u-strasbg.fr/cgi-bin/qcat?J/ A+A/.. Additional data not included in this article but part of the overall Gaiamoons occultation observation dataset will be avail- able in the thesis manuscript of the corresponding author that will be published in late 2026. aw data of this study are available from the corresponding author upon request. Acknowledgements. This work was supported by the project GaiaMoons of the Agence Nationale de Recherche (France), grant ANR-22-CE490002. The GaiaMoons team gratefully acknowledges the amateur communities of IOTA, IOTA/ES, IOTA/EA, TTOA, and Planoccult for their essential support, ded- ication, and significant contributions to this work. The properties of Solar System Object are from the service SsODNet.ssoCard of the Space Service (SE-OP) of Laboratoire Temps Espace at Paris Observatory through its So- lar System Portal (https://ssp.imcce.fr) (Berthier et al. 2023) with the python library rocks (https://github.com/maxmahlke/rocks). We made use of Astropy, a community-developed core Python package for Astron- omy (Astropy Collaboration et al. 2013). This work has made use of data from the European Space Agency (ESA) mission Gaia (https://www. cosmos.esa.int/Gaia), processed by the Gaia Data Processing and Anal- ysis Consortium (DPAC, https://www.cosmos.esa.int/web/Gaia/dpac/ consortium). The authors would like to thank the Action Pluriannuelle In- citative (API) Pro-Am initiated and supported by Paris Observatory in the ROADIES program context. Z. Liu and D. Hestroffer thank the Academie Spatial program for their support. Part of observations were funded by the Scientific Research Projects Coordination Unit of Istanbul University with project numbers: BAP-3685 and FBG-2017-23943. Felipe Braga-Ribas ac- knowledges CNPq grant 316604/2023-2 and the financial support of the NAPI “Fenômenos Extremos do Universo” of Fundação de Apoio à Ciência, Tecnologia e Inovação do Paraná. M.A. thanks grants CNPq 427700/2018- 3, 310683/2017-3, and 473002/2013-2, and FAPERJ E-26/210.705/2024. Y. Kilic, J.L. Ortiz, N. Morales and P. Santos-Sanz acknowledge financial support from the Severo Ochoa grant CEX2021-001131-S funded by MI- CIU/AEI/10.13039/501100011033. P. Santos-Sanz and Y. Kilic acknowledge fi- nancial support from the Spanish I+D+i project PID2022-139555NB-I00 (TNO- JWST) funded by MCIN/AEI/10.13039/501100011033. TUG100 Telescope at the Antalya TUG Site of the Türkiye National Observatories has been utilised, and we express our gratitude for the support provided by the Türkiye National Observatories and all its staff. The authors would like to thank the following ob- servers who participated and provided data for the events: R. Leiva, A. Ossola, A. Catapano, B. Lade, R. Prentice, S. Whitehurst, E. Goni, E. Namur Neto, J. Delin- cak, J. Talbot, J. A. Berlanga, J. Collada Barcena, K. Harrison, M. Skrutskie, M. Gutekunst, N. Karaman, N. Wakefield, V. Cucchiaro, X. Dupont, T. Legault, S. Kidd, P. Le Cam, J.-N. Ferrier, G. Vanwalleghem, E. Vauthrin, F. Thill, B. Lott, D. Tamonis, and A. Maury.
Detection and characterisation of binary asteroid candidates through stellar occultations · 2026 · DOIThe grainy and jumping migration scenarios proposed for Neptune (Nesvorný & Vokrouhlický 2016; Nesvorný & Morbidelli 2012) are mentioned as alternative to smooth exponential migration, but the paper provides no numerical simulations testing how discontinuous or episodic migration events affect capture efficiency and final population distributions in individual mean motion resonances.
The primordial planetesimal disk is inferred to extend to 60-70 au based on order-of-magnitude agreement between theory and observations for MMRs between 1:2 and 1:4, but this inference lacks direct observational constraints on the actual density profile and sharp density drop-off characteristics at these distances during the late stages of giant planet migration.
The discrepancy between theoretical predictions and observations for the 1:2 MMR is attributed to poorer resonant island stability and fragmentation at low inclinations, but the paper lacks direct frequency analysis calculations showing the eigenfrequency differences and dynamical timescale comparisons between the 1:2 and 2:3 MMRs under the same initial conditions.
The exponential migration model presented assumes that planetesimal density and eccentricity excitation (σe) are spatially uniform, but Equation 6 is noted to require extension when these parameters vary as functions of semimajor axis. The paper does not provide numerical implementations or results for how differential planetesimal density profiles across the primordial disk affect capture probabilities in different Neptune resonances.
The distant mean motion resonances beyond the 1:4 MMR (particularly the 1:6 MMR and others in that region) currently lack observational data and population estimates. The paper identifies that resonant sticking effects may dominate over Neptune migration capture in these regions, but no simulations directly compare capture predictions from migration-based mechanisms versus resonant sticking mechanisms at these remote semimajor axes.
The 3:4 and 4:5 mean motion resonances interior to the 1:2 MMR show theoretical predictions that consistently exceed observational values by more than the confidence intervals, yet the paper lacks specific dynamical stability analysis quantifying how proximity to Neptune affects resonant island fragmentation and long-term stability timescales for these inner resonances compared to the 2:3 MMR.
The constant migration rate model used for calculating capture into Neptune's mean motion resonances has not been validated against exponential decay migration patterns or grainy migration scenarios. The authors propose that their methodology can be extended to variable migration rates but provide only a preliminary exponential migration model example without numerical results comparing predicted populations against observations under these more realistic migration assumptions.
However, previous studies have yielded inconsistent results because the small sizes of the spectral features and the limited information content of the data resulted in high sensitivity to the varying assumptions made in the treatment of instrument systematics and the atmospheric retrieval analysis 3–12 .
Moreover, these reflected objects are out-of-rank, that is, they have not yet been determined with respect to the ranks of xenolandscape formations, similarly formed due to the synergy of influences and interactions of different strengths, but genetically the same initial xenolandscape-forming factors of material and energy-field xenonaturals.
They have been imaged at more than 285 unique locations from August 2018 (when the atmosphere was clearing as the PEDE decayed) to August 2019, about half (157) of which are locations where RSL have not been documented previously.
Mars: Abundant Recurring Slope Lineae (RSL) Following the Planet‐Encircling Dust Event (PEDE) of 2018 · 2021 · DOIUsing the lightcurve inversion method, the combination of our lightcurves and the sparse data from ATLAS{HKO and ATLAS-MLO, we also found the sidereal period, indicating a retrograde rotation of the asteroid, with two possible mirrored pole solutions.
**Causal Hypotheses:** The current evidence establishes spatial over-representation; determining whether this reflects early Holocene astronomical observation, deliberate geodetic design, environmental adaptation, or residual selection effects remains an open scientific question.
A Geometric Derivation of the 47.1° Vector: Spatial Clustering and Early Holocene Obliquity Correlations · 2026 · DOIAbstract There are many different theoretical explanations for the formation of high-density Mercury-like planets, but concrete evidence for any of these formation mechanisms remains elusive.
The Maximum Density of a Collisionally-Produced Planet is A Function of its Mass and Orbital Period · 2026 · DOINevertheless, embedding coupled magma-atmosphere models directly within Bayesian retrievals enables quantitative assessment of degeneracies and sensitivities, establishing a pathway for directly connecting atmospheric spectra to magma composition in this underexplored exoplanet regime.
Double-diffusive convection in the ``fuzzy'' cores of giant planets has been widely discussed as a mechanism for redistributing heavy elements, but its efficiency in evolutionary models remains uncertain.
Self-Consistent Evolution Models Show Weak Double-Diffusive Mixing in Jupiter and Saturn · 2026The early states of terrestrial planets are expected to be dominated by the thermal and rotational outcomes of giant impacts, but critical parameters that control internal processes, such as the pressures and temperatures of core formation, are not fully understood.
Thermal and rotational effects of giant impacts during terrestrial planet accretion · 2026There are limited data in the literature presenting Centaur colors in the SDSS filter system for a direct comparison with 450P.
JWST and Gemini Observations of the Active Centaur 450P/LONEOS: Nucleus and Coma Characterizations · 2026 · DOIThe physical and geochemical differences between Earth and Mars provide fundamental constraints on terrestrial planet formation, yet a self-consistent framework linking dynamical and chemical aspects remains elusive.
Coupling dynamical accretion and chemical differentiation: A unified framework for the diversity of Earth and Mars · 2026 · DOIWhile secondary processes related to atmospheric entry and post-impact evolution are investigated, quantitative constraints on P-T-time paths during these processes are not fully established.
A Petrographic and Micro-Analytical Framework for the Study and Classification of Meteorites · 2026 · DOIThe comparative framework among ordinary chondrites is developed but lacks systematic comparison with carbonaceous, enstatite, and achondritic meteorite groups.
A Petrographic and Micro-Analytical Framework for the Study and Classification of Meteorites · 2026 · DOI
Most-cited papers in Astro and Planetary Science
- Space weathering on airless bodies · Journal of Geophysical Research Planets · 2016 · 535 citations
- Asteroid (101955) Bennu in the laboratory: Properties of the sample collected by <scp>OSIRIS</scp>‐<scp>REx</scp> · Meteoritics and Planetary Science · 2024 · 191 citations
- Dust Growth and Evolution in Protoplanetary Disks · Annual Review of Astronomy and Astrophysics · 2024 · 121 citations
- Hot Jupiters: Origins, Structure, Atmospheres · Journal of Geophysical Research Planets · 2021 · 115 citations
- Aerosols in Exoplanet Atmospheres · Journal of Geophysical Research Planets · 2021 · 110 citations
- A high internal heat flux and large core in a warm Neptune exoplanet · Nature · 2024 · 108 citations
- Possible Hycean conditions in the sub-Neptune TOI-270 d · Astronomy and Astrophysics · 2024 · 105 citations
- A radius valley between migrated steam worlds and evaporated rocky cores · Nature Astronomy · 2024 · 104 citations
- The Composition and Chemistry of Titan’s Atmosphere · ACS Earth and Space Chemistry · 2024 · 91 citations
- JWST Observations of K2-18b Can Be Explained by a Gas-rich Mini-Neptune with No Habitable Surface · The Astrophysical Journal Letters · 2024 · 88 citations
Most recent work
- Postperihelion Integral Field Spectroscopy of the Interstellar Comet 3I/ATLAS · The Astrophysical Journal · 2026
- Detection of an atmosphere on a trans-Neptunian object beyond Pluto · Nature Astronomy · 2026
- Observations of the 2023 February 27 fireball in northern Sweden using the auroral imaging system ALIS_4D · Monthly Notices of the Royal Astronomical Society · 2026
- Comet Tail Analyzer: A GUI Tool for Finson–Probstein Dust-tail Modeling · Research Notes of the AAS · 2026
- The DART Mission and Advancements in Planetary Defense · Annual Review of Earth and Planetary Sciences · 2026
- The r-process: history, required conditions, astrophysical sites, and observations · The European Physical Journal A · 2026
- New 12C/13C and 14N/15N isotopic ratios measurements in HCN in the Jupiter stratosphere revealed by ALMA · Astronomy & Astrophysics · 2026
- A meteorite impact crater in the Eastern Goldfields of Western Australia—Shock metamorphism and projectile signature at the Ora Banda structure · Meteoritics & Planetary Science · 2026
- Visible, near‐, and thermal infrared spectra of asteroid Bennu samples: Relationship to and implications for remote sensing of carbonaceous asteroids · Meteoritics and Planetary Science · 2026
- On the tidal response of Titan inferred from Cassini data · Nature Astronomy · 2026
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