Literature DB >> 15448263

Solar wind-induced atmospheric erosion at Mars: first results from ASPERA-3 on Mars Express.

R Lundin1, S Barabash, H Andersson, M Holmström, A Grigoriev, M Yamauchi, J-A Sauvaud, A Fedorov, E Budnik, J-J Thocaven, D Winningham, R Frahm, J Scherrer, J Sharber, K Asamura, H Hayakawa, A Coates, D R Linder, C Curtis, K C Hsieh, B R Sandel, M Grande, M Carter, D H Reading, H Koskinen, E Kallio, P Riihela, W Schmidt, T Säles, J Kozyra, N Krupp, J Woch, J Luhmann, S McKenna-Lawler, R Cerulli-Irelli, S Orsini, M Maggi, A Mura, A Milillo, E Roelof, D Williams, S Livi, P Brandt, P Wurz, P Bochsler.   

Abstract

The Analyzer of Space Plasma and Energetic Atoms (ASPERA) on board the Mars Express spacecraft found that solar wind plasma and accelerated ionospheric ions may be observed all the way down to the Mars Express pericenter of 270 kilometers above the dayside planetary surface. This is very deep in the ionosphere, implying direct exposure of the martian topside atmosphere to solar wind plasma forcing. The low-altitude penetration of solar wind plasma and the energization of ionospheric plasma may be due to solar wind irregularities or perturbations, to magnetic anomalies at Mars, or both.

Entities:  

Year:  2004        PMID: 15448263     DOI: 10.1126/science.1101860

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  1 in total

1.  Carbon Ion Fluxes at Mars: First Results of Tailward Flows From MAVEN-STATIC.

Authors:  N B Pickett; J P McFadden; C M Fowler; K G Hanley; M Benna
Journal:  J Geophys Res Space Phys       Date:  2021-12-30       Impact factor: 3.111

  1 in total

北京卡尤迪生物科技股份有限公司 © 2022-2023.