Waves in the innermost open boundary layer formed by dayside magnetopause reconnection-Reference-Cited by-同舟云学术

Waves in the innermost open boundary layer formed by dayside magnetopause reconnection

Published:2017-03 Issue:3 Volume:122 Page:3291-3307
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res. Space Physics

Author:

Uchino H.¹,Kurita S.²^ORCID,Harada Y.³^ORCID,Machida S.²,Angelopoulos V.⁴

Affiliation:

1. Department of Geophysics, Graduate School of ScienceKyoto University Kyoto Japan

2. Institute for Space‐Earth Environmental ResearchNagoya University Nagoya Japan

3. Space Sciences LaboratoryUniversity of California Berkeley California USA

4. Department of Earth, Planetary, and Space Sciences and Institute of Geophysics and Planetary PhysicsUniversity of California Los Angeles California USA

Funder

National Aeronautics and Space Administration

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JA023300

Reference55 articles.

1. The THEMIS Mission

2. The THEMIS Fluxgate Magnetometer

3. The Electric Field Instrument (EFI) for THEMIS

4. chap. Reconnection at Earth's Dayside Magnetopause;Cassak P. A.,2016

5. The THEMIS Digital Fields Board

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