M. Slipski
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View article: Joint Observations of Mesospheric Aerosols on Mars from MAVEN/IUVS and MRO/MCS
Joint Observations of Mesospheric Aerosols on Mars from MAVEN/IUVS and MRO/MCS Open
JOINT OBSERVATIONS OF MESOSPHERIC AEROSOLS ON MARS FROM MAVEN/IUVS AND MRO/MCS Ashwin S. Braude1, Marek Slipski1, Sumedha Gupta2, Nicholas M. Schneider2, Armin Kleinböhl1, Franck Montmessin3, Sonal Jain2, Roger V. Yelle4 and Justin Deighan…
View article: Role of Thermal Tides and Gravity Waves in Mars Equatorial Mesospheric Cloud Formation Revealed by Mars Climate Sounder Observations
Role of Thermal Tides and Gravity Waves in Mars Equatorial Mesospheric Cloud Formation Revealed by Mars Climate Sounder Observations Open
Mesospheric CO 2 ‐ice clouds form in one of the coldest regions of Mars's atmosphere, but to date links between the broader thermal structure, dynamical phenomena, and the global and seasonal structure of mesospheric clouds have been tenta…
View article: Atmospheric Evolution of Mars Inferred from Argon Isotopes
Atmospheric Evolution of Mars Inferred from Argon Isotopes Open
Today, Mars is a cold, dry planet with a thin atmosphere, incapable of sustaining liquid water on the surface. However, there is ample evidence that liquid water once flowed on the surface, which could have been maintained by a warmer and …
View article: Variability of Martian Turbopause Altitudes
Variability of Martian Turbopause Altitudes Open
The turbopause and homopause represent the transition from strong turbulence and mixing in the middle atmosphere to a molecular‐diffusion‐dominated region in the upper atmosphere. We use neutral densities measured by the Neutral Gas and Io…
View article: Mars’ atmospheric history derived from upper-atmosphere measurements of <sup>38</sup> Ar/ <sup>36</sup> Ar
Mars’ atmospheric history derived from upper-atmosphere measurements of <sup>38</sup> Ar/ <sup>36</sup> Ar Open
Measurements of Mars’ atmosphere show that 66% has been lost to space, leading to changes in the planet’s climate.