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Published on: June 9, 2016
Observations of double layers in earth's plasma sheet
R E Ergun1, L Andersson, J Tao
1Department of Astrophysical and Planetary Sciences, University of Colorado, Boulder, Colorado 80309, USA.
Scientists observed parallel electric fields within double layers in Earth's plasma sheet. These findings suggest double layers are a universal process in space plasmas, indicating complex kinetic behaviors.
Area of Science:
- Space Physics
- Plasma Physics
- Magnetospheric Physics
Background:
- Double layers (DLs) are structures known to accelerate charged particles.
- Previous observations of parallel electric fields within DLs were primarily in Earth's auroral region.
- The plasma sheet is a dynamic region within Earth's magnetosphere, crucial for understanding space weather.
Purpose of the Study:
- To report the first direct observations of parallel electric fields (E_{ parallel}) associated with double layers (DLs) in Earth's magnetosphere plasma sheet.
- To investigate the occurrence and characteristics of DLs in different plasma sheet regions.
- To assess the implications of these observations for understanding plasma behavior in the magnetosphere.
Main Methods:
- Direct in-situ measurements by the THEMIS spacecraft.
- Analysis of electric field and plasma data within the magnetosphere's plasma sheet.
- Identification of double layer signatures during specific plasma phenomena.
Main Results:
- Direct observations of parallel electric fields (E_{ parallel}) carried by double layers (DLs) were made in the plasma sheet.
- DLs were observed in conjunction with bursty bulk flow events, the current sheet, and the plasma sheet boundary layer.
- The observed E_{ parallel} signals in the plasma sheet were analogous to those found in the auroral region.
Conclusions:
- Double layers (DLs) appear to be a universal phenomenon in Earth's magnetosphere, not limited to the auroral zone.
- The presence of DLs in the plasma sheet indicates that strongly nonlinear and kinetic plasma behaviors are intrinsic to this region.
- These findings enhance our understanding of energy transfer and particle acceleration processes within the magnetosphere.
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