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Atmospheric Science with InSight
Authors:Aymeric Spiga  Don Banfield  Nicholas A Teanby  François Forget  Antoine Lucas  Balthasar Kenda  Jose Antonio Rodriguez Manfredi  Rudolf Widmer-Schnidrig  Naomi Murdoch  Mark T Lemmon  Raphaël F Garcia  Léo Martire  Özgür Karatekin  Sébastien Le Maistre  Bart Van Hove  Véronique Dehant  Philippe Lognonné  Nils Mueller  Ralph Lorenz  David Mimoun  Sébastien Rodriguez  Éric Beucler  Ingrid Daubar  Matthew P Golombek  Tanguy Bertrand  Yasuhiro Nishikawa  Ehouarn Millour  Lucie Rolland  Quentin Brissaud  Taichi Kawamura  Antoine Mocquet  Roland Martin  John Clinton  Éléonore Stutzmann  Tilman Spohn  Suzanne Smrekar  William B Banerdt
Institution:1.Jet Propulsion Laboratory,California Institute of Technology,Pasadena,USA;2.Cornell Center for Astrophysics and Planetary Science,Cornell University,Ithaca,USA;3.NASA Ames Research Center,Mountain View,USA;4.Laboratoire de Planétologie et Géodynamique,Université de Nantes,Nantes,France;5.Division of Geological and Planetary Sciences,California Institute of Technology,Pasadena,USA;6.Institut Supérieur de l’Aéronautique et de l’Espace (ISAE-SUPAERO),Université de Toulouse,Toulouse,France;7.ETH,Zurich,Switzerland;8.Royal Observatory of Belgium,Brussels,Belgium;9.Laboratoire de Météorologie Dynamique (LMD/IPSL),Sorbonne Université, Centre National de la Recherche Scientifique, école Polytechnique, école Normale Supérieure,Paris,France;10.Institut de Physique du Globe de Paris,Université Paris Diderot,Paris,France;11.Texas A&M university,College Station,USA;12.Institut Universitaire de France,Paris,France;13.Applied Physics Laboratory,Johns Hopkins University,Laurel,USA;14.CAB,Madrid,Spain;15.Geoazur, Université C?te d’Azur,Observatoire de la C?te d’Azur,Nice,France;16.DLR, German Aerospace Center,Institute of Planetary Research,Berlin,Germany;17.School of Earth Sciences,University of Bristol,Bristol,UK;18.Institut für Geophysik,Universit?t Stuttgart,Stuttgart,Germany;19.Géoscience Environnement Toulouse, Observatoire midi-Pyrénées,Université de Toulouse,Toulouse,France
Abstract:In November 2018, for the first time a dedicated geophysical station, the InSight lander, will be deployed on the surface of Mars. Along with the two main geophysical packages, the Seismic Experiment for Interior Structure (SEIS) and the Heat-Flow and Physical Properties Package (HP3), the InSight lander holds a highly sensitive pressure sensor (PS) and the Temperature and Winds for InSight (TWINS) instrument, both of which (along with the InSight FluxGate (IFG) Magnetometer) form the Auxiliary Sensor Payload Suite (APSS). Associated with the RADiometer (RAD) instrument which will measure the surface brightness temperature, and the Instrument Deployment Camera (IDC) which will be used to quantify atmospheric opacity, this will make InSight capable to act as a meteorological station at the surface of Mars. While probing the internal structure of Mars is the primary scientific goal of the mission, atmospheric science remains a key science objective for InSight. InSight has the potential to provide a more continuous and higher-frequency record of pressure, air temperature and winds at the surface of Mars than previous in situ missions. In the paper, key results from multiscale meteorological modeling, from Global Climate Models to Large-Eddy Simulations, are described as a reference for future studies based on the InSight measurements during operations. We summarize the capabilities of InSight for atmospheric observations, from profiling during Entry, Descent and Landing to surface measurements (pressure, temperature, winds, angular momentum), and the plans for how InSight’s sensors will be used during operations, as well as possible synergies with orbital observations. In a dedicated section, we describe the seismic impact of atmospheric phenomena (from the point of view of both “noise” to be decorrelated from the seismic signal and “signal” to provide information on atmospheric processes). We discuss in this framework Planetary Boundary Layer turbulence, with a focus on convective vortices and dust devils, gravity waves (with idealized modeling), and large-scale circulations. Our paper also presents possible new, exploratory, studies with the InSight instrumentation: surface layer scaling and exploration of the Monin-Obukhov model, aeolian surface changes and saltation / lifing studies, and monitoring of secular pressure changes. The InSight mission will be instrumental in broadening the knowledge of the Martian atmosphere, with a unique set of measurements from the surface of Mars.
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