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Published on: May 19, 2014
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Two states of magnetotail dipolarization fronts: A statistical study
D Schmid1, R Nakamura2, F Plaschke2
1Space Research Institute, Austrian Academy of Sciences Graz, Austria ; University of Graz, NAWI Graz Graz, Austria.
Summary
Earth's magnetotail dipolarization fronts show diverse plasma sheet responses. While some fronts increase temperature and decrease density, others do the opposite, suggesting complex evolution of plasma flows after magnetic reconnection.
Area of Science:
- Space Physics
- Plasma Physics
- Earth's Magnetosphere
Background:
- Dipolarization fronts (DFs) are key features in the Earth's magnetotail.
- Previous studies suggested a consistent plasma sheet response across DFs.
Purpose of the Study:
- To statistically analyze ion density and temperature variations during DF crossings.
- To investigate the diverse plasma sheet responses associated with DFs.
Main Methods:
- Utilized 9 years of Cluster spacecraft data (2001-2009).
- Selected DFs with earthward plasma flow > 150 km/s.
- Performed statistical analysis of temperature and density changes across DFs.
Main Results:
- Identified two main categories of DF crossings: Category A (54%) with increasing temperature/decreasing density, and Category B (28%) with decreasing temperature/increasing density.
- Category A DFs showed a decrease in thermal pressure, especially on the duskside.
- Category B DFs exhibited different flow characteristics, background magnetic fields, and no clear pressure change pattern.
Conclusions:
- The study reveals a more complex picture of plasma sheet dynamics during DFs than previously thought.
- Hypothesizes that Category A flows evolve into Category B flows as they propagate earthward, indicating a developmental process post-reconnection.
Keywords:
dipolarization frontMore Related Videos
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