Characterizing magnetopause shadowing effects in the outer electron radiation belt during geomagnetic storms

2016 ◽  
Vol 121 (10) ◽  
pp. 9517-9530 ◽  
Author(s):  
D. Herrera ◽  
V. F. Maget ◽  
A. Sicard-Piet
Keyword(s):  
Radiation Belt ◽  
Geomagnetic Storms ◽  
Electron Radiation ◽  
Outer Electron ◽  
Shadowing Effects

scholarly journals The Response of the Energy Content of the Outer Electron Radiation Belt to Geomagnetic Storms

2018 ◽  
Vol 123 (10) ◽  
pp. 8227-8240 ◽  
Author(s):  
Ying Xiong ◽  
Lun Xie ◽  
Lunjin Chen ◽  
Binbin Ni ◽  
Suiyan Fu ◽  
...  
Keyword(s):  
Radiation Belt ◽  
Geomagnetic Storms ◽  
Energy Content ◽  
Electron Radiation ◽  
Outer Electron

scholarly journals A density-temperature description of the outer electron radiation belt during geomagnetic storms

2010 ◽  
Vol 115 (A1) ◽  
pp. n/a-n/a ◽  
Author(s):  
Michael H. Denton ◽  
Joseph E. Borovsky ◽  
Thomas E. Cayton
Keyword(s):  
Radiation Belt ◽  
Geomagnetic Storms ◽  
Electron Radiation ◽  
Outer Electron

scholarly journals Relative positions of the polar boundary of the outer electron radiation belt and the equatorial boundary of the auroral oval

2018 ◽  
Vol 36 (4) ◽  
pp. 1131-1140 ◽  
Author(s):  
Maria O. Riazanteseva ◽  
Elizaveta E. Antonova ◽  
Marina V. Stepanova ◽  
Boris V. Marjin ◽  
Ilia A. Rubinshtein ◽  
...  
Keyword(s):  
Radiation Belt ◽  
Geomagnetic Storms ◽  
Background Level ◽  
Auroral Oval ◽  
Electron Radiation ◽  
Outer Electron ◽  
Outer Radiation Belt ◽  
Auroral Electrons ◽  
The Difference ◽  
Scintillator Detectors

Abstract. Finding the position of the polar boundary of the outer electron radiation belt, relative to the position of the auroral oval, is a long-standing problem. Here we analyze it using the data of the METEOR-M1 auroral satellite for the period from 11 November 2009 to 27 March 2010. The geomagnetic conditions during the analyzed period were comparatively quiet. METEOR-M1 has a polar solar-synchronous circular orbit with an altitude of ≈832 km, a period of 101.3 min, and an inclination of 98∘. We analyze flux observations of auroral electrons with energies between 0.03 and 16 keV, and electrons with energies >100 keV, measured simultaneously by the GGAK-M set of instruments, composed of semiconductors, scintillator detectors, and electrostatic analyzers. We assume that in the absence of geomagnetic storms the polar boundary of the outer radiation belt can be identified as a decrease in the count rate of precipitating energetic electrons to the background level. It was found that this boundary can be located both inside the auroral oval or equatorward of the equatorial boundary of the auroral precipitation. It was also found that for slightly disturbed geomagnetic conditions the polar boundary of the outer radiation belt is almost always located inside the auroral oval. We observe that the difference between the position of the polar boundary of the outer radiation belt and the position of the equatorial boundary of the auroral precipitation depend on the AE and PC indices of geomagnetic activity. The implications of these results in the analysis of the formation of the outer radiation belt are discussed.

scholarly journals A relation between the locations of the polar boundary of outer electron radiation belt and the equatorial boundary of the auroral oval

2018 ◽  
Author(s):  
Maria O. Riazanteseva ◽  
Elizaveta E. Antonova ◽  
Marina V. Stepanova ◽  
Boris V. Marjin ◽  
Ilia A. Rubinshtein ◽  
...  
Keyword(s):  
Radiation Belt ◽  
Geomagnetic Storms ◽  
Outer Boundary ◽  
Background Level ◽  
Auroral Oval ◽  
External Boundary ◽  
Electron Radiation ◽  
Outer Electron ◽  
Outer Radiation Belt ◽  
The Difference

Abstract. Finding the position of the external boundary of the outer electron radiation belt, relative to the position of the auroral oval, is a long-standing problem. Here we analyze it using data of the Meteor-M No. 1 auroral satellite for the period from 11 November 2009 to 27 March 2010. The geomagnetic conditions during the analyzed period were comparatively quiet. Meteor-M No. 1 has a polar solar-synchronous circular orbit with an altitude of ~ 832 km, a period of 101.3 min, and an inclination of 98°. We analyze flux observations of auroral electrons with energies between 0.03 and 16 keV, and electrons with energies > 100 keV, measured simultaneously by the GGAK-M set of instruments, composed by semiconductors, scintillator detectors, and electrostatic analyzers. We assume that at the absence of geomagnetic storms the external boundary of the outer radiation belt can be identified as a decrease in the count rate of precipitating energetic electrons to the background level. It was found that this boundary can be located both inside the auroral oval or to the equator from the equatorial boundary of the auroral precipitations. It was also found that for disturbed geomagnetic conditions the external boundary of the outer radiation belt is almost always located inside the auroral oval. We observe that the difference between the position of the outer boundary of the outer radiation belt and the position of the equatorial boundary of auroral precipitations depends on the AE and PC indexes of geomagnetic activity. The implications of these results in the analysis of the formation of the outer radiation belt is discussed.

Toward dynamic modeling of the outer electron radiation belt

1990 ◽  
Vol 95 (A8) ◽  
pp. 12069 ◽  
Author(s):  
Y. T. Chiu ◽  
M. A. Rinaldi ◽  
R. W. Nightingale
Keyword(s):  
Dynamic Modeling ◽  
Radiation Belt ◽  
Electron Radiation ◽  
Outer Electron

scholarly journals Processes in auroral oval and outer electron radiation belt

2018 ◽  
Vol 70 (1) ◽  
Author(s):  
Elizaveta E. Antonova ◽  
Marina V. Stepanova ◽  
Pablo S. Moya ◽  
Victor A. Pinto ◽  
Vadim V. Vovchenko ◽  
...  
Keyword(s):  
Radiation Belt ◽  
Auroral Oval ◽  
Electron Radiation ◽  
Outer Electron
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