Wind retrieval from temperature measurements from the Rover Environmental Monitoring Station/Mars Science Laboratory

We are grateful to the entire MSL Curiosity rover team and to the REMS instrument team, in particular, for their work on the wind data on Mars, without which this research could not have been performed. MPZ has been partially funded by the Spanish State Research Agency (AEI) Project No. MDM-2017-073...

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Bibliographic Details
Published in:Icarus
Main Authors: Soria-Salinas, Álvaro, Zorzano, María-Paz, Mantas-Nakhai, Roberto, Martín-Torres, Javier
Other Authors: University of Aberdeen.Geology and Geophysics
Format: Article in Journal/Newspaper
Language:English
Published: 2020
Subjects:
Mars
Atmosphere
Meteorology
VIKING
MARTIAN DUST CYCLE
CONVECTION HEAT-TRANSFER
GALE CRATER
LAMINAR BOUNDARY-LAYER
CIRCULAR-CYLINDER
CROSS-FLOW
REMS
QE Geology
Astronomy and Astrophysics
Space and Planetary Science
QE
Luleå
Online Access:https://hdl.handle.net/2164/14096
https://doi.org/10.1016/j.icarus.2020.113785
http://www.scopus.com/inward/record.url?scp=85083241376&partnerID=8YFLogxK
http://www.sciencedirect.com/science/article/pii/S0019103520301718
Description
Summary:We are grateful to the entire MSL Curiosity rover team and to the REMS instrument team, in particular, for their work on the wind data on Mars, without which this research could not have been performed. MPZ has been partially funded by the Spanish State Research Agency (AEI) Project No. MDM-2017-0737 Unidad de Excelencia “María de Maeztu”- Centro de Astrobiología (CSIC-INTA). The resources used for the simulations presented in this work were provided by the Graduate School of Space Technology of Luleå University of Technology. We give special thanks to Ricardo M. Fonseca for his useful comments and suggestions on this work that extended the horizons of this research from the beginning. Peer reviewed

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