A Comparative Study of Magnetic Flux Ropes in the Nightside Induced Magnetosphere of Mars and Venus-Reference-Cited by-同舟云学术

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A Comparative Study of Magnetic Flux Ropes in the Nightside Induced Magnetosphere of Mars and Venus

Published:2022-01 Issue:1 Volume:127 Page:
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:JGR Space Physics

Author:

Hara Takuya¹^ORCID,Huang Zesen¹²³^ORCID,Mitchell David L.¹^ORCID,DiBraccio Gina A.⁴^ORCID,Brain David A.⁵^ORCID,Harada Yuki⁶^ORCID,Luhmann Janet G.¹

Affiliation:

1. Space Sciences Laboratory University of California Berkeley Berkeley CA USA

2. University of Science and Technology of China Hefei China

3. Department of Earth, Planetary and Space Sciences University of California Los Angeles Los Angeles CA USA

4. NASA Goddard Space Flight Center Greenbelt MD USA

5. Laboratory for Atmospheric and Space Physics University of Colorado Boulder Boulder CO USA

6. Department of Geophysics Kyoto University Kyoto Japan

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JA029867

Reference63 articles.

1. Global Distribution of Crustal Magnetization Discovered by the Mars Global Surveyor MAG/ER Experiment

2. The Space Physics Environment Data Analysis System (SPEDAS)

3. MAVEN Survey of Magnetic Flux Rope Properties in the Martian Ionosphere: Comparison With Three Types of Formation Mechanisms

4. Climates of terrestrial planets

5. Martian magnetic morphology: Contributions from the solar wind and crust

Cited by 3 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Magnetic Reconnection at Planetary Bodies and Astrospheres;Space Science Reviews;2024-01-19

2. Three‐Dimensional Configuration of Induced Magnetic Fields Around Mars;Journal of Geophysical Research: Planets;2022-08

3. Heavy Ion Escape From Martian Wake Enhanced by Magnetic Reconnection;Journal of Geophysical Research: Planets;2022-05-30

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