The NetLander MagNet experiment

In the frame of the NetLander mission, developed by an European consortium under CNES leadership, a network of 4 landers will be deployed at the Mars surface. Among other instruments, the geophysical package of each lander will include a magnetometer. The different possible contributions of magnetic...

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Main Authors: Menvielle, Michel, Primdahl, F., Brauer, P., Jensen, P.A., Merayo, J.M.G., Berthelier, Jean-Jacques, Breuer, Doris, Chanteur, Gérard, Mandea, M., Magnes, Werner, Musmann, G., Pajunpaa, K., Pinçon, Jean-Louis, Schwingenschuh, Konrad, Szarka, L., Vennerstrøm, S.
Other Authors: Centre d'étude des environnements terrestre et planétaires (CETP), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS), Danish Space Research Institute (DSRI), DTU Electrical Engineering Lyngby, Danmarks Tekniske Universitet = Technical University of Denmark (DTU), National Space Institute Lyngby (DTU Space), Deutsches Zentrum für Luft- und Raumfahrt (DLR), Centre National d'Études Spatiales Toulouse (CNES), Austrian Academy of Sciences (OeAW), Technische Universität Braunschweig = Technical University of Braunschweig Braunschweig, Finnish Meteorological Institute (FMI), Laboratoire de physique et chimie de l'environnement (LPCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS), Geodetic and Geophysical Research Institute (GGRI), Research Centre for Astronomy and Earth Sciences Budapest, Hungarian Academy of Sciences (MTA)-Hungarian Academy of Sciences (MTA), P. Stauning (ed.)
Format: Conference Object
Language:English
Published: HAL CCSD 2002
Subjects:
Online Access:https://hal.science/hal-00155823
id ftuniversailles:oai:HAL:hal-00155823v1
record_format openpolar
institution Open Polar
collection Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ
op_collection_id ftuniversailles
language English
topic [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[PHYS.PHYS.PHYS-PLASM-PH]Physics [physics]/Physics [physics]/Plasma Physics [physics.plasm-ph]
spellingShingle [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[PHYS.PHYS.PHYS-PLASM-PH]Physics [physics]/Physics [physics]/Plasma Physics [physics.plasm-ph]
Menvielle, Michel
Primdahl, F.
Brauer, P.
Jensen, P.A.
Merayo, J.M.G.
Berthelier, Jean-Jacques
Breuer, Doris
Chanteur, Gérard
Mandea, M.
Magnes, Werner
Musmann, G.
Pajunpaa, K.
Pinçon, Jean-Louis
Schwingenschuh, Konrad
Szarka, L.
Vennerstrøm, S.
The NetLander MagNet experiment
topic_facet [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph]
[PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO]
[PHYS.PHYS.PHYS-PLASM-PH]Physics [physics]/Physics [physics]/Plasma Physics [physics.plasm-ph]
description In the frame of the NetLander mission, developed by an European consortium under CNES leadership, a network of 4 landers will be deployed at the Mars surface. Among other instruments, the geophysical package of each lander will include a magnetometer. The different possible contributions of magnetic measurements onboard the NetLander stations are presented. The MagNet consists in continuous recording of the transient variations in the three components of the magnetic field observed at each NetLander. The transient variations of the magnetic field at the surface of a planet has a primary external source, the interaction between the environment of the planet and solar radiation, and a secondary source, the electric currents induced in the conductive planet. The continuous recording of the time variations of the magnetic fields at the surface of Mars by means of three component magnetometers installed onboard NetLander stations will therefore allow study of both the internal structure of Mars and the dynamic of its ionised environment. As is the case for the Earth, different possible controling plasma processes will lead to different convection patterns inside the magnetosphere and therefore different magnetic signatures at the planetary surface. Continuous recordings of the transient variations of the magnetic field onboard landers will then provide constraints on the convection within the Martian magnetosphere, that is a small magnetosphere where the ionosphere lies at great heights relative to the dimensions of the magnetospheric cavity. The use of the network magnetic data to probe the internal structure of Mars is also considered. The information that can be thus obtained on the Mars permafrost, lithosphere and mantle structure illustrated by numerical simulations. Finally, the specifications of the instrument allowing to achieve these objectives are discussed, and the instrument described.
author2 Centre d'étude des environnements terrestre et planétaires (CETP)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)
Danish Space Research Institute (DSRI)
DTU Electrical Engineering Lyngby
Danmarks Tekniske Universitet = Technical University of Denmark (DTU)
National Space Institute Lyngby (DTU Space)
Deutsches Zentrum für Luft- und Raumfahrt (DLR)
Centre National d'Études Spatiales Toulouse (CNES)
Austrian Academy of Sciences (OeAW)
Technische Universität Braunschweig = Technical University of Braunschweig Braunschweig
Finnish Meteorological Institute (FMI)
Laboratoire de physique et chimie de l'environnement (LPCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS)
Geodetic and Geophysical Research Institute (GGRI)
Research Centre for Astronomy and Earth Sciences Budapest
Hungarian Academy of Sciences (MTA)-Hungarian Academy of Sciences (MTA)
P. Stauning (ed.)
format Conference Object
author Menvielle, Michel
Primdahl, F.
Brauer, P.
Jensen, P.A.
Merayo, J.M.G.
Berthelier, Jean-Jacques
Breuer, Doris
Chanteur, Gérard
Mandea, M.
Magnes, Werner
Musmann, G.
Pajunpaa, K.
Pinçon, Jean-Louis
Schwingenschuh, Konrad
Szarka, L.
Vennerstrøm, S.
author_facet Menvielle, Michel
Primdahl, F.
Brauer, P.
Jensen, P.A.
Merayo, J.M.G.
Berthelier, Jean-Jacques
Breuer, Doris
Chanteur, Gérard
Mandea, M.
Magnes, Werner
Musmann, G.
Pajunpaa, K.
Pinçon, Jean-Louis
Schwingenschuh, Konrad
Szarka, L.
Vennerstrøm, S.
author_sort Menvielle, Michel
title The NetLander MagNet experiment
title_short The NetLander MagNet experiment
title_full The NetLander MagNet experiment
title_fullStr The NetLander MagNet experiment
title_full_unstemmed The NetLander MagNet experiment
title_sort netlander magnet experiment
publisher HAL CCSD
publishDate 2002
url https://hal.science/hal-00155823
op_coverage Copenhagen, Denmark
genre permafrost
genre_facet permafrost
op_source OIST-4 Proceedings 4th Oersted International Science Team Conference
https://hal.science/hal-00155823
OIST-4 Proceedings 4th Oersted International Science Team Conference, Sep 2002, Copenhagen, Denmark. pp.301-304
op_relation hal-00155823
https://hal.science/hal-00155823
_version_ 1772818861042696192
spelling ftuniversailles:oai:HAL:hal-00155823v1 2023-07-30T04:06:19+02:00 The NetLander MagNet experiment Menvielle, Michel Primdahl, F. Brauer, P. Jensen, P.A. Merayo, J.M.G. Berthelier, Jean-Jacques Breuer, Doris Chanteur, Gérard Mandea, M. Magnes, Werner Musmann, G. Pajunpaa, K. Pinçon, Jean-Louis Schwingenschuh, Konrad Szarka, L. Vennerstrøm, S. Centre d'étude des environnements terrestre et planétaires (CETP) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) Danish Space Research Institute (DSRI) DTU Electrical Engineering Lyngby Danmarks Tekniske Universitet = Technical University of Denmark (DTU) National Space Institute Lyngby (DTU Space) Deutsches Zentrum für Luft- und Raumfahrt (DLR) Centre National d'Études Spatiales Toulouse (CNES) Austrian Academy of Sciences (OeAW) Technische Universität Braunschweig = Technical University of Braunschweig Braunschweig Finnish Meteorological Institute (FMI) Laboratoire de physique et chimie de l'environnement (LPCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université d'Orléans (UO)-Centre National de la Recherche Scientifique (CNRS) Geodetic and Geophysical Research Institute (GGRI) Research Centre for Astronomy and Earth Sciences Budapest Hungarian Academy of Sciences (MTA)-Hungarian Academy of Sciences (MTA) P. Stauning (ed.) Copenhagen, Denmark 2002-09 https://hal.science/hal-00155823 en eng HAL CCSD hal-00155823 https://hal.science/hal-00155823 OIST-4 Proceedings 4th Oersted International Science Team Conference https://hal.science/hal-00155823 OIST-4 Proceedings 4th Oersted International Science Team Conference, Sep 2002, Copenhagen, Denmark. pp.301-304 [SDU.ASTR]Sciences of the Universe [physics]/Astrophysics [astro-ph] [PHYS.ASTR.CO]Physics [physics]/Astrophysics [astro-ph]/Cosmology and Extra-Galactic Astrophysics [astro-ph.CO] [PHYS.PHYS.PHYS-PLASM-PH]Physics [physics]/Physics [physics]/Plasma Physics [physics.plasm-ph] info:eu-repo/semantics/conferenceObject Conference papers 2002 ftuniversailles 2023-07-16T21:18:41Z In the frame of the NetLander mission, developed by an European consortium under CNES leadership, a network of 4 landers will be deployed at the Mars surface. Among other instruments, the geophysical package of each lander will include a magnetometer. The different possible contributions of magnetic measurements onboard the NetLander stations are presented. The MagNet consists in continuous recording of the transient variations in the three components of the magnetic field observed at each NetLander. The transient variations of the magnetic field at the surface of a planet has a primary external source, the interaction between the environment of the planet and solar radiation, and a secondary source, the electric currents induced in the conductive planet. The continuous recording of the time variations of the magnetic fields at the surface of Mars by means of three component magnetometers installed onboard NetLander stations will therefore allow study of both the internal structure of Mars and the dynamic of its ionised environment. As is the case for the Earth, different possible controling plasma processes will lead to different convection patterns inside the magnetosphere and therefore different magnetic signatures at the planetary surface. Continuous recordings of the transient variations of the magnetic field onboard landers will then provide constraints on the convection within the Martian magnetosphere, that is a small magnetosphere where the ionosphere lies at great heights relative to the dimensions of the magnetospheric cavity. The use of the network magnetic data to probe the internal structure of Mars is also considered. The information that can be thus obtained on the Mars permafrost, lithosphere and mantle structure illustrated by numerical simulations. Finally, the specifications of the instrument allowing to achieve these objectives are discussed, and the instrument described. Conference Object permafrost Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ