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Mars Soil Temperature and Thermal Properties from InSight HP 3 Data
  • +9
  • Tilman Spohn,
  • N Müller,
  • J Knollenberg,
  • M Grott,
  • M P Golombek,
  • A.-C Plesa,
  • V T Bickel,
  • P Morgan,
  • C Krause,
  • D Breuer,
  • S E Smrekar,
  • W B Banerdt
Tilman Spohn
Institute of Planetary Research, German Aerospace Center DLR

Corresponding Author:[email protected]

Author Profile
N Müller
Institute of Planetary Research, German Aerospace Center DLR
J Knollenberg
Institute of Planetary Research, German Aerospace Center DLR
M Grott
Institute of Planetary Research, German Aerospace Center DLR
M P Golombek
Jet Propulsion Laboratory, California Institute of Technology
A.-C Plesa
Institute of Planetary Research, German Aerospace Center DLR
V T Bickel
Center for Space and Habitability, University of Bern
P Morgan
Colorado Geological Survey, Colorado School of Mines
C Krause
MUSC Space Operations and Astronaut Training, German Aerospace Center DLR
D Breuer
Institute of Planetary Research, German Aerospace Center DLR
S E Smrekar
Jet Propulsion Laboratory, California Institute of Technology
W B Banerdt
Jet Propulsion Laboratory, California Institute of Technology

Abstract

• We measured the temperature and its diurnal and annual variations in the top 40cm of the Martian soil at the InSight landing site • The soil thermal diffusivity was calculated from the diurnal and seasonal surface and soil temperature variations • The soil temperature allows the formation of thin films of brine; their efflorescence may explain the formation of the observed duricrust
05 Sep 2024Submitted to ESS Open Archive
05 Sep 2024Published in ESS Open Archive
28 Sep 2024Published in Geophysical Research Letters volume 51 issue 18. 10.1029/2024GL108600