The ion temperature gradient: An intrinsic property of Earth's magnetotail-Reference-Cited by-同舟云学术

The ion temperature gradient: An intrinsic property of Earth's magnetotail

Published:2017-08 Issue:8 Volume:122 Page:8295-8309
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res. Space Physics

Author:

Lu San¹^ORCID,Artemyev A. V.¹²^ORCID,Angelopoulos V.¹,Lin Y.³^ORCID,Wang X. Y.³^ORCID

Affiliation:

1. Department of Earth, Planetary, and Space Sciences and Institute of Geophysics and Planetary Physics; University of California; Los Angeles California USA

2. Space Research Institute; RAS; Moscow Russia

3. Department of Physics; Auburn University; Auburn Alabama USA

Funder

National Aeronautics and Space Administration

German Ministry for Economy and Technology

Deutsches Zentrum für Luft- und Raumfahrt

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017JA024209/fullpdf

Reference63 articles.

1. The THEMIS mission;Angelopoulos;Space Sci. Rev.,2008

2. Thin embedded current sheets: Cluster observations of ion kinetic structure and analytical models;Artemyev;Ann. Geophys.,2009

3. Proton velocity distribution in thin current sheets: Cluster observations and theory of transient trajectories;Artemyev;J. Geophys. Res.,2010

4. Cluster statistics of thin current sheets in the Earth magnetotail: Specifics of the dawn flank, proton temperature profiles and electrostatic effects;Artemyev;J. Geophys. Res.,2011

5. Ion resonance acceleration by dipolarization fronts: Analytic theory and spacecraft observation;Artemyev;Ann. Geophys.,2012

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