Journal article
The polar cusp location and its dependence on dipole tilt
Geophysical research letters, Vol.26(3), pp.429-432
1999
DOI: 10.1029/1998GL900312
Abstract
Polar cusp crossings at high altitudes are seen in the POLAR data as decreases in the magnetic field and increases in magnetosheath-like plasma. Close to 500 polar cusp crossings identified from the magnetic field, low-energy electron and ion data observed by POLAR, are used to determine the statistical location of the polar cusp. When compared with Tsyganenko's 1989 vacuum model with an ellipsoidal magnetopause [Tsyganenko, 1989], the medians of the cusp crossings are located between the magnetic field lines with invariant latitudes of 80° and 82°. Statistically the shape of the polar cusp in this region is consistent with this model although there is much scatter around the median value. The position of the cusp is significantly dependent on the dipole tilt angle. When dipole tilts more toward the Sun, the cusp moves more poleward to higher invariant latitude from 77.2° at −30° tilt, to 80.0° at 0° tilt, to 81.8° at 30° or roughly 1° for every 14° of tilt.
Details
- Title: Subtitle
- The polar cusp location and its dependence on dipole tilt
- Creators
- X.-W Zhou - University of California, Los AngelesC. T Russell - University of California, Los AngelesG LE - University of California, Los AngelesS. A Fuselier - Lockheed MartinJ. D Scudder - University of Iowa
- Resource Type
- Journal article
- Publication Details
- Geophysical research letters, Vol.26(3), pp.429-432
- Publisher
- American Geophysical Union
- DOI
- 10.1029/1998GL900312
- ISSN
- 0094-8276
- eISSN
- 1944-8007
- Language
- English
- Date published
- 1999
- Academic Unit
- Physics and Astronomy
- Record Identifier
- 9984199665902771
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