Localized Heating of the Martian Topside Ionosphere Through the Combined Effects of Magnetic Pumping by Large‐Scale Magnetosonic Waves and Pitch Angle Diffusion by Whistler Waves-Reference-Cited by-同舟云学术

Localized Heating of the Martian Topside Ionosphere Through the Combined Effects of Magnetic Pumping by Large‐Scale Magnetosonic Waves and Pitch Angle Diffusion by Whistler Waves

Published:2020-03-03 Issue:5 Volume:47 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Fowler C. M.¹^ORCID,Agapitov O. V.¹^ORCID,Xu S.¹^ORCID,Mitchell D. L.¹^ORCID,Andersson L.²^ORCID,Artemyev A.³^ORCID,Espley J.⁴^ORCID,Ergun R. E.²^ORCID,Mazelle C.⁵^ORCID

Affiliation:

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

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

3. Institute of Geophysics and Planetary Physics University of California, Los Angeles Los Angeles CA USA

4. NASA Goddard Space Flight Center Greenbelt MD USA

5. IRAP, University of Toulouse‐CNRS‐UPS‐CNES Toulouse France

Funder

National Aeronautics and Space Administration

National Science Foundation

Publisher

American Geophysical Union (AGU)

Subject