Soil Thermophysical Properties Near the InSight Lander Derived From 50 Sols of Radiometer Measurements

Autor: John A. Grant, Veronique Ansan, Nicholas H. Warner, Matthew P. Golombek, Bruce Banerdt, Nils Müller, Justin N. Maki, Matthias Grott, Tilman Spohn, Mark T. Lemmon, Susan Smrekar, Nathan R. Williams, François Forget, Ehouarn Millour, Ingrid Daubar, Matthew A. Siegler, Aymeric Spiga, Don Banfield, Jörg Knollenberg, Sylvain Piqueux
Přispěvatelé: Jet Propulsion Laboratory (JPL), NASA-California Institute of Technology (CALTECH), Deutsches Zentrum für Luft- und Raumfahrt [Berlin] (DLR), Planetary Science Institute [Tucson] (PSI), Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-École normale supérieure - Paris (ENS Paris), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL), Texas A&M University [College Station]
Jazyk: angličtina
Rok vydání: 2021
Předmět:
Zdroj: Journal of Geophysical Research. Planets
Journal of Geophysical Research. Planets, Wiley-Blackwell, 2021, 126 (8), ⟨10.1029/2021JE006859⟩
ISSN: 2169-9097
2169-9100
Popis: Measurements from the InSight lander radiometer acquired after landing are used to characterize the thermophysical properties of the Martian soil in Homestead hollow. This data set is unique as it stems from a high measurement cadence fixed platform studying a simple well-characterized surface, and it benefits from the environmental characterization provided by other instruments. We focus on observations acquired before the arrival of a regional dust storm (near Sol 50), on the furthest observed patch of soil (i.e., ∼3.5 m away from the edge of the lander deck) where temperatures are least impacted by the presence of the lander and where the soil has been least disrupted during landing. Diurnal temperature cycles are fit using a homogenous soil configuration with a thermal inertia of 183 ± 25 J m
Databáze: OpenAIRE