Strong ambipolar-driven ion upflow within the cleft ion fountain during low geomagnetic activity-Reference-Cited by-同舟云学术

Strong ambipolar-driven ion upflow within the cleft ion fountain during low geomagnetic activity

Published:2016-07 Issue:7 Volume:121 Page:6950-6969
ISSN:2169-9380
Container-title:Journal of Geophysical Research: Space Physics
language:en
Short-container-title:J. Geophys. Res. Space Physics

Author:

Shen Yangyang¹,Knudsen David J.¹,Burchill Johnathan K.¹^ORCID,Howarth Andrew¹,Yau Andrew¹^ORCID,Redmon Robert J.²,Miles David M.³^ORCID,Varney Roger H.⁴,Nicolls Michael J.⁴

Affiliation:

1. Department of Physics and Astronomy; University of Calgary; Calgary Alberta Canada

2. National Centers for Environmental Information; Boulder Colorado USA

3. Department of Physics; University of Alberta; Edmonton Alberta Canada

4. SRI International; Menlo Park California USA

Funder

Eyes High Doctoral Recruitment Scholarship

University of Calgary

Natural Sciences and Engineering Research Council of Canada

Canadian Space Agency

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2016JA022532/fullpdf

Reference72 articles.

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3. Transverse ion energization and wave emissions observed by the Freja satellite;André;Geophys. Res. Lett.,1994

4. Initial ionospheric observations made by the new Resolute incoherent scatter radar and comparison to solar wind IMF;Bahcivan;Geophys. Res. Lett.,2010

5. On the altitude dependence of transversely heated O+ distributions in the cusp/cleft;Bouhram;Ann. Geophys.,2004

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