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Observations of the South Polar Residual Cap suggest a possible erosion of the cap, leading to an increase of the global mass of the atmosphere. We test this assumption by making the first comparison between Viking 1 and InSight surface…

地球与行星天体物理 · 物理学 2022-09-28 L. Lange , F. Forget , D. Banfield , M. Wolff , A. Spiga , E. Millour , D. Viúdez-Moreiras , A. Bierjon , S. Piqueux , C. Newman , J. Pla-García , W. B. Banerdt

Crater chronologies are a fundamental tool to assess relative and absolute ages of planetary surfaces when direct radiometric dating is not available. Martian crater chronologies are derived from lunar crater spatial densities on terrains…

地球与行星天体物理 · 物理学 2021-03-24 Simone Marchi

For decades, scientists have tried to explain the evidence for fluvial activity on early Mars, but a consensus has yet to emerge regarding the mechanism for producing it. One hypothesis suggests early Mars was warmed by a thick greenhouse…

地球与行星天体物理 · 物理学 2016-11-21 Natasha E. Batalha , Ravi K. Kopparapu , Jacob Haqq-Misra , James F. Kasting

Mars is the Solar System's canonical small, rocky planet that transitioned from early geologic activity and surface liquid water to a cold and arid planet with a thin, cold, CO$_2$-dominated atmosphere. The evolution of Mars, in the context…

The two moons of Mars, Phobos and Deimos, have orbits that are close to martian equator, indicating their formation from a circumplanetary disk. Phobos is currently migrating toward Mars due to tidal dissipation within the planet, and may…

地球与行星天体物理 · 物理学 2025-03-18 Matija Ćuk , Kaustub P. Anand , David A. Minton

Soil assessment is important for mobile robot planning and navigation on natural and planetary environments. Terramechanic characteristics can be inferred from the thermal behaviour of soils under the influence of sunlight using remote…

The detection of geologically recent channels at the end of the twentieth century rapidly suggested that liquid water could have been present on Mars up to recent times. A mechanism involving melting of water ice during ice ages in the last…

地球与行星天体物理 · 物理学 2015-12-17 Mathieu Vincendon

The dynamics of Mars' obliquity are believed to be chaotic, and the historical ~3.5 Gyr (late-Hesperian onward) obliquity probability density function (PDF) is high uncertain and cannot be inferred from direct simulation alone. Obliquity is…

地球与行星天体物理 · 物理学 2019-04-19 Samuel J. Holo , Edwin S. Kite , Stuart J. Robbins

Computing the tidal deformations of Mars, we explored various Mars internal structures by examining profiles that include or exclude a basal molten layer within the mantle and a solid inner core. By assessing their compatibility with a…

地球与行星天体物理 · 物理学 2024-03-12 Alex Guinard , Agnes Fienga , Anthony Memin , Clement Ganino

Martian surface morphology implies that Mars was once warm enough to maintain persistent liquid water on its surface. While the high D/H ratios (~6 times the Earth's ocean water) of the current martian atmosphere suggest that significant…

地球与行星天体物理 · 物理学 2015-06-19 Hiroyuki Kurokawa , Masahiko Sato , Masashi Ushioda , Takeshi Matsuyama , Ryota Moriwaki , James M. Dohm , Tomohiro Usui

Mars' sedimentary rocks record Gyrs of environmental change. New data enable the first global analysis of paleo-environment relevant physical properties of these rocks, including layer thickness and accumulation rate. We find that layer…

地球与行星天体物理 · 物理学 2025-03-04 Madison L. Turner , Sabrina Y. Khan , Kevin W. Lewis , Axel Noblet , Edwin S. Kite

Remote sensing data from orbiter missions have proposed that ground ice may currently exist on Mars, although the volume is still uncertain. Recent analyses of Martian meteorites have suggested that the water reservoirs have at least three…

地球与行星天体物理 · 物理学 2015-11-11 Hiroyuki Kurokawa , Tomohiro Usui , Masahiko Sato

Ancient sediments provide archives of climate and habitability on Mars. Gale Crater, the landing site for the Mars Science Laboratory (MSL), hosts a 5 km high sedimentary mound. Hypotheses for mound formation include evaporitic, lacustrine,…

地球与行星天体物理 · 物理学 2012-07-06 Edwin S. Kite , Kevin W. Lewis , Michael P. Lamb

In this chapter we begin with a review of Titan's fluvial and lacustrine landscapes as observed with Cassini remote sensing data, and what the many discoveries have revealed about Titan's surface materials and climate. Yet Cassini remote…

地球与行星天体物理 · 物理学 2025-02-05 Samuel P. D. Birch , Alexander G. Hayes , J. Taylor Perron

Planetary surfaces are typically analyzed using high-level semantic concepts in natural language, yet vast orbital image archives remain organized at the pixel level. This mismatch limits scalable, open-ended exploration of planetary…

We review the abundance and diversity of terrestrial rock hosted life, the environments it inhabits, the evolution of its metabolisms, and its fossil biomarkers to provide guidance in the search for the biomarkers of rock hosted life on…

地球与行星天体物理 · 物理学 2019-10-16 T. C. Onstott , B. L. Ehlmann , H. Sapers , M. Coleman , M. Ivarsson , J. J. Marlow , A. Neubeck , P. Niles

Much of the geologic activity preserved on Europa's icy surface has been attributed to tidal deformation, mainly due to Europa's eccentric orbit. Although the surface is geologically young (30 - 80 Myr), there is little information as to…

地球与行星天体物理 · 物理学 2015-06-24 Alyssa R. Rhoden , Terry A. Hurford , Lorenz Roth , Kurt Retherford

The present article proposes an approach to analyze the photometric properties of the surface materials from multi-angle observations acquired by the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) on-board the Mars…

地球与行星天体物理 · 物理学 2014-08-25 J. Fernando , F. Schmidt , X. Ceamanos , P. Pinet , S. Douté , Y Daydou