Mars‐solar wind interaction: LatHyS, an improved parallel 3‐D multispecies hybrid model
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- Ronan Modolo
- LATMOS/IPSL, UVSQ Université Paris‐Saclay, UPMC University Paris CNRS Guyancourt France
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- Sebastien Hess
- LATMOS/IPSL, UVSQ Université Paris‐Saclay, UPMC University Paris CNRS Guyancourt France
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- Marco Mancini
- LATMOS/IPSL, UVSQ Université Paris‐Saclay, UPMC University Paris CNRS Guyancourt France
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- Francois Leblanc
- LATMOS/IPSL, UPMC University Paris 06 Sorbonne Universités, UVSQ, CNRS Paris France
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- Jean‐Yves Chaufray
- LATMOS/IPSL, UPMC University Paris 06 Sorbonne Universités, UVSQ, CNRS Paris France
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- David Brain
- LASP University of Colorado Boulder Boulder Colorado USA
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- Ludivine Leclercq
- LATMOS/IPSL, UVSQ Université Paris‐Saclay, UPMC University Paris CNRS Guyancourt France
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- Rosa Esteban‐Hernández
- LATMOS/IPSL, UPMC University Paris 06 Sorbonne Universités, UVSQ, CNRS Paris France
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- Gerard Chanteur
- LPP Ecole Polytechnique Palaiseau France
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- Philippe Weill
- LATMOS/IPSL, UPMC University Paris 06 Sorbonne Universités, UVSQ, CNRS Paris France
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- Francisco González‐Galindo
- IAA Granada Spain
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- Francois Forget
- LMD/UPMC/CNRS Paris France
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- Manabu Yagi
- LATMOS/IPSL, UPMC University Paris 06 Sorbonne Universités, UVSQ, CNRS Paris France
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- Christian Mazelle
- LATMOS/IPSL, UVSQ Université Paris‐Saclay, UPMC University Paris CNRS Guyancourt France
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説明
<jats:title>Abstract</jats:title><jats:p>In order to better represent Mars‐solar wind interaction, we present an unprecedented model achieving spatial resolution down to 50 km, a so far unexplored resolution for global kinetic models of the Martian ionized environment. Such resolution approaches the ionospheric plasma scale height. In practice, the model is derived from a first version described in Modolo et al. (2005). An important effort of parallelization has been conducted and is presented here. A better description of the ionosphere was also implemented including ionospheric chemistry, electrical conductivities, and a drag force modeling the ion‐neutral collisions in the ionosphere. This new version of the code, named LatHyS (Latmos Hybrid Simulation), is here used to characterize the impact of various spatial resolutions on simulation results. In addition, and following a global model challenge effort, we present the results of simulation run for three cases which allow addressing the effect of the suprathermal corona and of the solar EUV activity on the magnetospheric plasma boundaries and on the global escape. Simulation results showed that global patterns are relatively similar for the different spatial resolution runs, but finest grid runs provide a better representation of the ionosphere and display more details of the planetary plasma dynamic. Simulation results suggest that a significant fraction of escaping O<jats:sup>+</jats:sup> ions is originated from below 1200 km altitude.</jats:p>
収録刊行物
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- Journal of Geophysical Research: Space Physics
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Journal of Geophysical Research: Space Physics 121 (7), 6378-6399, 2016-07
American Geophysical Union (AGU)
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詳細情報 詳細情報について
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- CRID
- 1364233269580513024
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- ISSN
- 21699402
- 21699380
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- データソース種別
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- Crossref
- OpenAIRE