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Record W4399489229 · doi:10.1038/s41561-024-01457-7

Evidence for transient morning water frost deposits on the Tharsis volcanoes of Mars

2024· article· en· W4399489229 on OpenAlexaff
Adomas Valantinas, N. Thomas, A. Pommerol, Özgür Karatekin, Luca Ruiz Lozano, Cem Berk Senel, Orkun Temel, Ernst Hauber, Daniela Tirsch, Valentin Bickel, Giovanni Munaretto, M. Pajola, Fabrizio Oliva, Frédéric Schmidt, Ian Thomas, A. S. McEwen, Miguel Almeida, Matthew Read, Vidhya Ganesh Rangarajan, M. R. El‐Maarry, Cristina Re, F. G. Carrozzo, E. D’Aversa, Frank Daerden, Bojan Ristic, Manish Patel, G. Bellucci, J. J. López‐Moreno, Ann Carine Vandaele, G. Cremonese

Bibliographic record

VenueNature Geoscience · 2024
Typearticle
Languageen
FieldPhysics and Astronomy
TopicPlanetary Science and Exploration
Canadian institutionsWestern University
FundersInstituto de Astrofísica de AndalucíaVlaamse regeringInstitut national des sciences de l'UniversFonds Wetenschappelijk OnderzoekCentre National d’Etudes SpatialesUniversity of BernCentre National de la Recherche ScientifiqueBelgian Federal Science Policy OfficeAgencia Estatal de InvestigaciónNational Aeronautics and Space Administration
KeywordsTharsisGeologyVolcanoMartianMars Exploration ProgramCalderaAstrobiologyImpact craterFrost (temperature)HesperianAtmospheric sciencesEarth scienceGeomorphologyGeochemistry

Abstract

fetched live from OpenAlex

Abstract The present-day water cycle on Mars has implications for habitability and future human exploration. Water ice clouds and water vapour have been detected above the Tharsis volcanic province, suggesting the active exchange of water between regolith and atmosphere. Here we report observational evidence for extensive transient morning frost deposits on the calderas of the Tharsis volcanoes (Olympus, Arsia and Ascraeus Montes, and Ceraunius Tholus) using high-resolution colour images from the Colour and Stereo Surface Imaging System on board the European Space Agency’s Trace Gas Orbiter. The transient bluish deposits appear on the caldera floor and rim in the morning during the colder Martian seasons but are not present by afternoon. The presence of water frost is supported by spectral observations, as well as independent imagery from the European Space Agency’s Mars Express orbiter. Climate model simulations further suggest that early-morning surface temperatures at the high altitudes of the volcano calderas are sufficiently low to support the daily condensation of water—but not CO 2 —frost. Given the unlikely seasonal nature of volcanic outgassing, we suggest the observed frost is atmospheric in origin, implying the role of microclimate in local frost formation and a contribution to the broader Mars water cycle.

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame distilled prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.000
Version: codex-gemma-dda1882f352aValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Bench or experimental · Consensus signal: Bench or experimental
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.125
Threshold uncertainty score0.161

Codex and Gemma teacher scores by category

CategoryCodexGemma
Metaresearch0.0000.000
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0000.000
Science and technology studies0.0000.000
Scholarly communication0.0000.000
Open science0.0000.000
Research integrity0.0000.000
Insufficient payload (model declined to judge)0.0000.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.029
GPT teacher head0.268
Teacher spread0.239 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one teacher head, not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designBench or experimental
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations11
Published2024
Admission routes1
Has abstractyes

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