The characteristics of the magnetopause reconnection X‐line deduced from low‐altitude satellite observations of cusp ions
Open Access
- 7 December 1994
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 21 (24) , 2757-2760
- https://doi.org/10.1029/94gl02696
Abstract
No abstract availableKeywords
This publication has 10 references indexed in Scilit:
- Low and middle altitude cusp particle signatures for general magnetopause reconnection rate variations: 1. TheoryJournal of Geophysical Research, 1994
- Model of magnetosheath plasma in the magnetosphere: Cusp and mantle particles at low‐altitudesGeophysical Research Letters, 1993
- The variation of reconnection rate at the dayside magnetopause and cusp ion precipitationJournal of Geophysical Research, 1992
- Ion distributions at the dayside magnetopauseJournal of Geophysical Research, 1991
- Ion Reflection and transmission during reconnection at the Earth's subsolar magnetopauseGeophysical Research Letters, 1991
- Cold ion beams in the low latitude boundary layer during accelerated flow eventsGeophysical Research Letters, 1990
- The causes of convection in the Earth's magnetosphere: A review of developments during the IMSReviews of Geophysics, 1982
- Evidence of magnetospheric cusp proton acceleration by magnetic merging at the dayside magnetopauseJournal of Geophysical Research, 1977
- Heos 2 plasma observations in the distant polar magnetosphere: The plasma mantleJournal of Geophysical Research, 1975
- Hydromagnetic flow around the magnetospherePlanetary and Space Science, 1966