Article
Multidisciplinary Sciences
Masayuki Naito, Hiroki Kusano, Satoshi Kodaira
Summary: Dose assessment on the lunar surface is crucial for future long-term crewed missions. In addition to galactic cosmic rays, neutrons and gamma-rays are generated by nuclear interactions and natural radioactive nuclides on the Moon. By utilizing simulations and measurement data, neutron and gamma-ray dose distributions on the Moon were obtained. The distributions varied depending on lunar geological features, with the basalt-rich mare having higher neutron dose rates and gamma-ray dose maps similar to the distribution of natural radioactive elements.
SCIENTIFIC REPORTS
(2023)
Article
Multidisciplinary Sciences
Riley Culberg, Dustin M. Schroeder, Gregor Steinbrugge
Summary: The formation mechanism of double ridges on Europa remains unclear. This study analyzes landforms on the Greenland Ice Sheet and suggests that the refreezing of shallow water sills may be responsible for the formation of these ridges. The findings indicate that the same process might be widespread across Europa's ice shell.
NATURE COMMUNICATIONS
(2022)
Article
Computer Science, Information Systems
Zhu Hong Lin, Shuai S. A. Yuan, Kai Li
Summary: The investigation of radiation field in the moon, specifically the vertical magnetic dipoles (VMD), is crucial for moon subsurface detection. This study focuses on analyzing the radiation field produced by VMD located on or near the moon's surface. The researchers derived analytical expressions using an approximate method and considered contributions from low-order and high-order terms. The proposed method and formulas have applications in moon interior exploration.
Article
Geosciences, Multidisciplinary
Ya Huei Huang, Jason M. Soderblom, David A. Minton, Masatoshi Hirabayashi, H. Jay Melosh
Summary: The porosity of the lunar crust can be used to determine the Moon's bombardment history. Lunar crustal porosity was largely generated early in lunar evolution and has decreased after that time. Additionally, the study suggests that the terrestrial planets experienced periods of high crustal porosity early in their evolution.
Article
Astronomy & Astrophysics
A. P. Jordan
Summary: Space weathering on the Moon is not only caused by solar wind and micrometeoroid impacts, but also by large solar energetic particle events. A combination of dielectric breakdown and micrometeoroid weathering can explain variations in lunar soil reflectance and the formation of magnetic anomalies on the Moon's surface.
Review
Astronomy & Astrophysics
F. Leblanc, C. Schmidt, V Mangano, A. Mura, G. Cremonese, J. M. Raines, J. M. Jasinski, M. Sarantos, A. Milillo, R. M. Killen, S. Massetti, T. Cassidy, R. J. Vervack, S. Kameda, M. T. Capria, M. Horanyi, D. Janches, A. Berezhnoy, A. Christou, T. Hirai, P. Lierle, J. Morgenthaler
Summary: This paper reviews the observations of sodium and potassium exospheres on Mercury and the Moon, discusses their sources and sinks, and highlights the role of magnetospheres. It also suggests new directions for research in understanding these exospheres.
SPACE SCIENCE REVIEWS
(2022)
Article
Geosciences, Multidisciplinary
Yunzhao Wu, Ekkehard Kuhrt, Matthias Grott, Qi Jin, Tianyi Xu, Jorn Helbert, Maximilian Hamm, Nannan Qin, Jinsong Ma, Jean-Baptiste Vincent, Paul Hayne
Summary: Temperature measurements on the lunar surface at centimeter scales in short-wavelength infrared were observed in situ by the Chang'E-4 rover, providing additional information to existing large-scale data. Surface roughness at subresolution scales was found to affect the observed thermal radiances and derived temperatures, highlighting the importance of considering this factor when determining the thermal properties of lunar regolith.
GEOPHYSICAL RESEARCH LETTERS
(2021)
Article
Engineering, Aerospace
M. Hirabayashi, C. M. Hartzell, P. M. Bellan, D. Bodewits, G. L. Delzanno, T. W. Hyde, U. Konopka, E. Thomas, H. M. Thomas, I. Hahn, U. E. Israelsson
Summary: Dust accumulation is a critical issue in lunar explorations. A team has been organized to define key science questions and assess dust remediation techniques. Three electrostatic remediation technology concepts have been investigated, and further development is needed.
Article
Astronomy & Astrophysics
Rachael M. Marshal, Ottaviano Ruesch, Christian Woehler, Kay Wohlfarth, Sergey Velichko
Summary: The study and investigation of meter and sub-meter scale geological features, especially boulders and boulder fields, on the surface of airless bodies can provide insight into the evolution of the regolith and the contribution of various processes to its formation. Prior studies have examined the photometric properties of the lunar regolith surrounding young craters using image ratios. We extend this methodology to extracting surface properties, in particular the roughness characteristics, exclusive to boulder fields and the boulders that constitute them around impact craters.
Article
Astronomy & Astrophysics
P. O. Hayne, O. Aharonson, N. Schorghofer
Summary: Water ice is believed to be trapped in large permanently shadowed regions in the lunar polar regions, but recent studies have revealed the presence of numerous small-scale cold traps, significantly expanding the areas where ice may accumulate. The majority of cold traps for water ice are found at latitudes greater than 80 degrees, with permanent shadows equatorward of 80 degrees typically too warm for ice accumulation to occur. This suggests that water resources at the lunar poles may be more widespread and accessible than previously thought.
Article
Astronomy & Astrophysics
A. B. Cunje, A. J. Dombard, R. R. Ghent
Summary: Larger impact craters and basins on the Moon show a discrepancy in crater size frequency distributions between their interior melt surfaces and exterior ejecta blankets. Despite elevated thermal conditions favorable to relaxation, simulations suggest that other mechanisms are likely responsible for the discrepancy in ages between the melt and ejecta surfaces.
Article
Astronomy & Astrophysics
A. P. Jordan, J. K. Wilson, H. E. Spence
Summary: Water ice in permanently shadowed regions on the moon is exposed to cosmic rays and solar energetic particles. Measuring the radiation dose is important for understanding the origin and evolution of the ice. The Cosmic Ray Telescope for the Effects of Radiation onboard the Lunar Reconnaissance Orbiter has provided valuable data on radiation in the lunar environment. Combining this data with a model for impact gardening, researchers have found that the dose received by impact-gardened ice is lower than previously estimated.
Article
Geosciences, Multidisciplinary
Huicun He, Jianglong Ji, Yue Zhang, Sen Hu, Yangting Lin, Hejiu Hui, Jialong Hao, Ruiying Li, Wei Yang, Hengci Tian, Chi Zhang, Mahesh Anand, Romain Tartese, Lixin Gu, Jinhua Li, Di Zhang, Qian Mao, Lihui Jia, Xiaoguang Li, Yi Chen, Li Zhang, Huaiwei Ni, Shitou Wu, Hao Wang, Qiuli Li, Huaiyu He, Xianhua Li, Fuyuan Wu
Summary: Analysis of lunar soils returned by the Chang'e-5 mission suggests that impact glass beads on the Moon's surface may contain a significant amount of solar wind-derived water. This finding supports the existence of a hydrated layer in lunar soils that plays a role in the global water cycle on the Moon. The study also reveals that impact glass beads can serve as reservoirs for water on other airless bodies.
Article
Astronomy & Astrophysics
C. D. Neish, K. M. Cannon, L. L. Tornabene, R. L. Flemming, M. Zanetti, E. Pilles
Summary: Researchers investigated impact melt deposits from seven lunar craters and found that their unique surface texture might be caused by a mixture of pyroxene and/or glassy material.
Article
Astronomy & Astrophysics
Emerson J. Speyerer, Mark S. Robinson, Aaron Boyd, Victor H. Silva, Samuel Lawrence
Summary: The UVVIS camera on the Clementine spacecraft provided a global, multispectral view of the Moon. Cross-mission comparisons were impaired by spatial offsets between the derived products. With new data from the LRO and GRAIL missions, image-based feature-matching algorithms were used to improve the positional accuracy of the UVVIS observations with the LROC WAC basemap, resulting in a foundational geospatial data product that aligns with the current lunar reference frame.
Article
Geochemistry & Geophysics
S. N. Valencia, B. L. Jolliff, R. L. Korotev
METEORITICS & PLANETARY SCIENCE
(2019)
Article
Geochemistry & Geophysics
Alian Wang, Yuanchao Yan, Bradley L. Jolliff, Scott M. McLennan, Kun Wang, Erbin Shi, William M. Farrell
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2020)
Article
Geochemistry & Geophysics
Zhen Tian, Bradley L. Jolliff, Randy L. Korotev, Bruce Fegley, Katharina Lodders, James M. D. Day, Heng Chen, Kun Wang
GEOCHIMICA ET COSMOCHIMICA ACTA
(2020)
Article
Geochemistry & Geophysics
Kelsi N. Singer, Bradley L. Jolliff, William B. McKinnon
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2020)
Review
Geochemistry & Geophysics
Alexander A. Nemchin, Tao Long, Bradley L. Jolliff, Yusheng Wan, Joshua F. Snape, Ryan Zeigler, Marion L. Grange, Dunyi Liu, Martin J. Whitehouse, Nicholas E. Timms, Fred Jourdan
Summary: This study presents new U-Pb ages for Apollo 14 and other lunar breccia samples, suggesting that the Imbrium impact occurred approximately 3922 million years ago. Results indicate that 36 samples can be interpreted as representing the formation of the Imbrium basin, supporting the conclusion that Imbrium material was widely distributed across the near side of the Moon. Additionally, 10 samples with ages about 50 million years younger than 3922 million years may represent a separate single impact event on the Moon, warranting further investigation to enhance our understanding of lunar impact history.
Article
Geochemistry & Geophysics
Alian Wang, Yuanchao Yan, Darby M. Dyar, Jen L. Houghton, William M. Farrell, Bradley L. Jolliff, Scott M. McLennan, Erbin Shi, Hongkun Qu
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2020)
Article
Geochemistry & Geophysics
Xiaohui Fu, Xuting Hou, Jiang Zhang, Bo Li, Zongcheng Ling, Bradley L. Jolliff, Lin Xu, Yongliao Zou
Summary: The CE-5 mission retrieved lunar regolith samples from the northern Oceanus Procellarum (NOP), revealing the presence of non-mare lithologies near the landing site. Chemical analysis identified different compositional groups within the region and suggested the influence of impact mixing on the lunar surface.
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2021)
Article
Geochemistry & Geophysics
K. L. Utt, R. C. Ogliore, H. A. Bechtel, J. J. Gillis-Davis, B. L. Jolliff
Summary: Space weathering processes alter the physical, chemical, and optical properties of space-exposed soil grains, particularly on the Moon. Super-resolution spectroscopic techniques offer a better understanding of the optical effects of space weathering on sub-micrometer length scales. The study found consistency with prior observations and models of space weathered spectra, providing a direct link between physical/chemical changes on grain surfaces and spectral changes of space weathered bodies.
JOURNAL OF GEOPHYSICAL RESEARCH-PLANETS
(2021)
Article
Geochemistry & Geophysics
Mason Neuman, Astrid Holzheid, Katharina Lodders, Bruce Fegley, Bradley L. Jolliff, Piers Koefoed, Heng Chen, Kun Wang
Summary: The study conducted twenty heating experiments to investigate the behavior of K, Cu, and Zn evaporation and isotopic fractionation from basaltic melts at high temperatures. Results show that Zn is the most volatile element followed by Cu and K. However, partitioning of Zn into spinel layers affects the Zn isotope fractionation factor. Higher temperatures and lower oxygen fugacities promote evaporation, and the experimentally determined fractionation factors for K and Cu are significantly larger than the apparent observed fractionation factors from lunar basalts.
GEOCHIMICA ET COSMOCHIMICA ACTA
(2022)
Article
Multidisciplinary Sciences
Xiaochao Che, Alexander Nemchin, Dunyi Liu, Tao Long, Chen Wang, Marc D. Norman, Katherine H. Joy, Romain Tartese, James Head, Bradley Jolliff, Joshua F. Snape, Clive R. Neal, Martin J. Whitehouse, Carolyn Crow, Gretchen Benedix, Fred Jourdan, Zhiqing Yang, Chun Yang, Jianhui Liu, Shiwen Xie, Zemin Bao, Runlong Fan, Dapeng Li, Zengsheng Li, Stuart G. Webb
Summary: By analyzing the youngest basalt lavas on the Moon, scientists have determined their age to be 1963 million years. This finding provides important constraints on the formation history and thermal evolution of the Moon. Additionally, there is no evidence for high concentrations of heat-producing elements in the deep mantle of the Moon, suggesting the need for alternative mechanisms to explain the continuous formation of lunar magmatism.
Article
Astronomy & Astrophysics
Jian Chen, Zongcheng Ling, Bradley L. Jolliff, Lingzhi Sun, Le Qiao, Jianzhong Liu, Xiaohui Fu, Jiang Zhang, Bo Li, Changqing Liu, Xiaobin Qi, Xuejin Lu, Zhiping He, Rui Xu
Summary: The Chang'e-4 mission landed in the Von Karman basaltic zone affected by Finse ejecta from the South Pole-Aitken (SPA) compositional anomaly (SPACA). A study using a mineral abundance unmixing model showed that the plagioclase abundance of SPACA exceeds the mineralogical range of SPA impact melt differentiation products, suggesting a contribution from crustal materials.
ASTROPHYSICAL JOURNAL LETTERS
(2022)
Article
Astronomy & Astrophysics
K. A. Mistick, R. N. Watkins, B. L. Jolliff, R. R. Ghent, R. L. Korotev, R. A. Zeigler
Summary: Using LROC NAC images, the boulder distribution around Vaughan crater on the far side of the Moon is analyzed, indicating that the crater is very young and a potential source of lunar meteorite Dhofar 961.
Article
Geochemistry & Geophysics
Amanda C. Stadermann, Bradley L. Jolliff, Michael J. Krawczynski, Christopher W. Hamilton, Jessica J. Barnes
Summary: Sample 12032,366-18 is a basaltic rock fragment collected during the Apollo 12 mission, enriched in incompatible trace elements such as Th, but not classified as a KREEP basalt. It may represent Th-rich mare basalts within Oceanus Procellarum, based on remote sensing data, with a major mineral assemblage of pyroxene, plagioclase, olivine, and ilmenite. The sample contains a Si-K-rich mesostasis, potentially formed by silicate liquid immiscibility, and experiments show the bulk composition reflects the magma it crystallized from.
METEORITICS & PLANETARY SCIENCE
(2022)
Article
Astronomy & Astrophysics
Xiaohui Fu, Chengxiang Yin, Bradley L. Jolliff, Jiang Zhang, Jian Chen, Zongcheng Ling, Feng Zhang, Yang Liu, Yongliao Zou
Summary: The Chang'E-5 mission successfully returned 1731 g of lunar soil and conducted a comparative study with Apollo and Luna soils, revealing similarities in mineralogy and geochemistry. The CE-5 soil represents a unique type of mare soil with high-FeO, intermediate-TiO2, and elevated incompatible elements. It expands the diversity of lunar samples and provides additional calibration soils for lunar remote sensing. The study also suggests a fractional crystallization history for the CE-5 mare basalt, similar to the Apollo high-Ti basalts.
Meeting Abstract
Geochemistry & Geophysics
X. Che, J. F. Snape, R. Tartese, K. H. Joy, Y. Shi, S. Xie, T. Long, A. A. Nemchin, M. D. Norman, C. R. Neal, J. Head, B. Jolliff, M. J. Whitehouse, Z. Bao, D. Liu
METEORITICS & PLANETARY SCIENCE
(2022)
Article
Astronomy & Astrophysics
Maria Angeles Lopez-Cayuela, Maria-Paz Zorzano, Juan Luis Guerrero-Rascado, Carmen Cordoba-Jabonero
Summary: The atmospheric dust cycle on Mars plays a dominant role in the planetary radiative balance, atmospheric photochemistry escape, and redistribution of materials on the surface. A methodology is presented to accurately describe the annual dust redistribution cycle on Mars using orbital global and seasonal measurements of atmospheric dust opacity. The analysis shows that approximately 4 trillion kilograms of dust is transported globally in the atmosphere during a typical Mars year.
Article
Astronomy & Astrophysics
Audrey Vorburger, Shahab Fatemi, Shane R. Carberry Mogan, Andre Galli, Lucas Liuzzo, Andrew R. Poppe, Lorenz Roth, Peter Wurz
Summary: The study presents new model results for the composition of Ganymede's atmosphere, finding that sublimation remains the major source process for H2O, while radiolysis induced by auroral electrons dominates the source fluxes for O2 and H2.
Article
Astronomy & Astrophysics
Qi He, Zhi Cao, Yuqi Qian, Hejiu Hui, Ioannis Baziotis, Long Xiao, Zaicong Wang, Biji Luo, Yiheng Li, Zongjun Ying, Yang Li
Summary: The Chang'e-5 mission collected lunar soil containing magnesian troctolitic granulites, which provide valuable information on the composition of the lunar crust. Through analysis and modeling, it is suggested that these granulites may have originated from the Pythagoras crater and were transported to the landing site.
Article
Astronomy & Astrophysics
Jordan M. Bretzfelder, Kathryn M. Stack, Abigail A. Fraeman, Mackenzie Day, William E. Dietrich, Alexander B. Bryk
Summary: This study investigates the development of bedrock ridges on Mars and their implications for wind history, deposition, and erosion in Gale crater.
Article
Astronomy & Astrophysics
Lot Ram, Diptiranjan Rout, Rahul Rathi, Paul Withers, Sumanta Sarkhel
Summary: This study investigates the impacts of interplanetary coronal mass ejections (ICMEs) on the Martian ionosphere, specifically the behavior of the ionospheric peak density and height during ICME passages. The study used observations from the Radio Occultation Science Experiment (ROSE) aboard the MAVEN spacecraft and selected 8 ICMEs from existing catalogs. The results show that ICMEs lead to an elevation of the ionospheric peak height and a decrease in peak density, and propose that vertical pressure gradient and electron temperature enhancement are plausible causes for ionospheric variability.
Article
Astronomy & Astrophysics
Benoit Jabaud, Riccardo Artoni, Gabriel Tobie, Erwan Le Menn, Patrick Richard
Summary: The Cassini spacecraft discovered active jets of water vapour and ice grains at the South Pole of Enceladus, resulting in the deposit of freshly erupted materials on the moon's icy surface. Similar processes may be happening on Europa as well. Determining the mechanical properties of fresh icy powder-like materials is essential for future landing and sampling missions. The flowability and surface energy of ice powders decrease with increasing temperatures, which may have implications for stable landing and the flow of ice materials on Enceladus and Europa.
Article
Astronomy & Astrophysics
Lydie Bonal, Eric Quirico, Gilles Montagnac, Mutsumi Komatsu, Yoko Kebukawa, Hikaru Yabuta, Kana Amano, Jens Barosch, Laure Bejach, George D. Cody, Emmanuel Dartois, Alexandre Dazzi, Bradley De Gregorio, Ariane Deniset-Besseau, Jean Duprat, Cecile Engrand, Minako Hashiguchi, Kanami Kamide, David Kilcoyne, Zita Martins, Jeremie Mathurin, Smail Mostefaoui, Larry Nittler, Takuji Ohigashi, Taiga Okumura, Laurent Remusat, Scott Sandford, Miho Shigenaka, Rhonda Stroud, Hiroki Suga, Yoshio Takahashi, Yasuo Takeichi, Yusuke Tamenori, Maximilien Verdier-Paoletti, Shohei Yamashita, Tomoki Nakamura, Hiroshi Naraoka, Takaaki Noguchi, Ryuji Okazaki, Hisayoshi Yurimoto, Shogo Tachibana, Masanao Abe, Akiko Miyazaki, Aiko Nakato, Satoru Nakazawa, Masahiro Nishimura, Tatsuaki Okada, Takanao Saiki, Kanako Sakamoto, Satoshi Tanaka, Fuyuto Terui, Yuichi Tsuda, Tomohiro Usui, Sei-ichiro Watanabe, Toru Yada, Kasumi Yogata, Makota Yoshikawa
Summary: This paper focuses on characterizing the thermal history of asteroid Ryugu by studying the structure of polyaromatic carbonaceous matter in the returned samples. The study finds that there is no structural difference in the polyaromatic component between the two sampling sites on Ryugu, indicating that the thermal metamorphism related to radioactive decay was not significant. However, some structural variability is observed within the particle set.
Article
Astronomy & Astrophysics
M. Luginin, A. Fedorova, D. Belyaev, F. Montmessin, O. Korablev, J. -l. Bertaux
Summary: Spectroscopic solar occultation measurements by the SPICAV/SOIR instrument onboard the Venus Express orbiter provided new data on the upper haze aerosol properties, its distribution, and variations. A joint analysis of data from two spectrometers revealed a bimodal distribution in about 50% of observations previously believed to be unimodal, and characterized the size distribution 10 km higher in the atmosphere compared to previous analysis.
Article
Astronomy & Astrophysics
A. Mahieux, S. Viscardy, K. L. Jessup, F. P. Mills, L. Trompet, S. Robert, S. Aoki, A. Piccialli, A. C. Vandaele
Summary: We report on the mean upper limit number densities and volume concentrations of H2CO, O-3, NH3, HCN, N2O, NO2, NO, and HO2 at the Venus terminator above the cloud layer. Attempts to detect these species using a statistical algorithm and the method presented by Trompet et al. (2021) were unsuccessful, and upper limits of detection are provided.
Article
Astronomy & Astrophysics
P. M. Streeter, S. R. Lewis, M. R. Patel, J. A. Holmes, K. Rajendran
Summary: The northern polar vortex on Mars shows a high degree of interannual repeatability in its structure and evolution, except during large dust storms. The seasonal timing of these storms seems to be the key factor determining their impacts on the polar vortex.
Article
Astronomy & Astrophysics
Michael T. Mellon, Hanna G. Sizemore, Jennifer L. Heldmann, Christopher P. McKay, Carol R. Stoker
Summary: The search for life is a major focus of Mars exploration, with temperature and water activity being key factors for habitability. The most recent habitable conditions occurred about 510 kyrs ago and lasted for about 10s of kyrs each occurrence. All latitudes offer potential for life exploration, but middle-latitude sites have access to 100-kyr-old ice that experienced past habitable conditions, while high-latitude sites offer access to ancient ice over 1 Myrs old.
Article
Astronomy & Astrophysics
Anthony Ozerov, Jeffrey C. Smith, Jessie L. Dotson, Randolph S. Longenbaugh, Robert L. Morris
Summary: The Geostationary Lightning Mapper (GLM) instruments, with their large combined field of view, are useful for studying the population of atmospheric phenomena like bolides. However, there are biases when using GLM for non-lightning purposes, which need to be studied and accounted for before precise measurements of bolide flux can be obtained. A Bayesian Poisson regression model was developed to estimate instrumental biases and the latitudinal variation of bolide flux concurrently. The estimated bias corresponds to the known sensitivity of the GLM instruments, and the latitudinal flux variation estimates are consistent with a strong bias towards high-velocity bolides, as compared to existing theoretical models.
Article
Astronomy & Astrophysics
P. Beck, P. Y. Meslin, A. Fau, O. Forni, O. Gasnault, J. Lasue, A. Cousin, S. Schroeder, S. Maurice, W. Rapin, R. C. Wiens, A. M. Ollila, E. Dehouck, N. Mangold, B. Garcia, S. Schwartz, W. Goetz, N. Lanza
Summary: Analysis of data obtained by ChemCam on Mars reveals that the carbon signal is mainly related to ionization of the atmosphere, with variability potentially linked to the physical state of the atmosphere. Up to sol 3355, no carbonate was detected in the ChemCam dataset, suggesting that it is not a major constituent (>50%) in the analyzed targets and that carbon in soils is not enriched beyond the limit of detection. The dominant salts found in Gale are sulfate and chlorides, while the absence of carbonates, seen in Jezero, may be due to differences in protolith.
Article
Astronomy & Astrophysics
Eloy Pena-Asensio, Jaakko Visuri, Josep M. Trigo-Rodriguez, Hector Socas-Navarro, Maria Gritsevich, Markku Siljama, Albert Rimola
Summary: The observation of interstellar objects 1I/'Oumuamua and 2I/Borisov suggests the existence of a larger population of smaller projectiles that impact our planet with unbound orbits. A statistical evaluation of uncertainties in the CNEOS database and study of its hyperbolic fireballs reveals an anisotropic geocentric radiant distribution and low orbital inclinations, challenging the assumption of a randomly incoming interstellar population. These findings suggest that apparent interstellar meteors may, in fact, be the result of accelerated meteoroid impacts caused by close encounters with massive objects within or passing through our solar system.
Article
Astronomy & Astrophysics
Cecilia W. S. Leung, Leslie K. Tamppari, David M. Kass, German Martinez, Erik Fischer, Michael D. Smith
Summary: Using a combination of orbital and surface observations, this study investigates the vertical distribution of water vapor in the lower atmospheres of Mars. The findings suggest that the assumption of uniformly mixed water vapor in the boundary layer is not always consistent with observational constraints. The results provide important insights into the seasonal transport of water and the role of regolith-atmospheric exchange.