scholarly journals Heppa III intercomparison experiment on electron precipitation impacts, part II: Model‐measurement intercomparison of nitric oxide (NO) during a geomagnetic storm in April 2010

Author(s):  
M. Sinnhuber ◽  
H. Nesse Tyssoy ◽  
T. Asikainen ◽  
S. Bender ◽  
B. Funke ◽  
...  
2012 ◽  
Vol 39 (21) ◽  
pp. n/a-n/a ◽  
Author(s):  
M. Daae ◽  
P. Espy ◽  
H. Nesse Tyssøy ◽  
D. Newnham ◽  
J. Stadsnes ◽  
...  

2007 ◽  
Vol 112 (A11) ◽  
pp. n/a-n/a ◽  
Author(s):  
Craig J. Rodger ◽  
Mark A. Clilverd ◽  
Neil R. Thomson ◽  
Rory J. Gamble ◽  
Annika Seppälä ◽  
...  

2019 ◽  
Vol 124 (3) ◽  
pp. 2113-2126 ◽  
Author(s):  
Zheng Li ◽  
Delores Knipp ◽  
Wenbin Wang

2007 ◽  
Vol 25 (9) ◽  
pp. 2053-2068 ◽  
Author(s):  
N. Longden ◽  
F. Honary ◽  
A. J. Kavanagh ◽  
J. Manninen

Abstract. The arrival of an interplanetary coronal mass ejection (ICME) triggered a sudden storm commencement (SSC) at ~09:22 UT on the 7 January 2005. The ICME followed a quiet period in the solar wind and interplanetary magnetic field (IMF). We present global scale observations of energetic electron precipitation during the moderate geomagnetic storm driven by the ICME. Energetic electron precipitation is inferred from increases in cosmic noise absorption (CNA) recorded by stations in the Global Riometer Array (GLORIA). No evidence of CNA was observed during the first four hours of passage of the ICME or following the sudden commencement (SC) of the storm. This is consistent with the findings of Osepian and Kirkwood (2004) that SCs will only trigger precipitation during periods of geomagnetic activity or when the magnetic perturbation in the magnetosphere is substantial. CNA was only observed following enhanced coupling between the IMF and the magnetosphere, resulting from southward oriented IMF. Precipitation was observed due to substorm activity, as a result of the initial injection and particles drifting from the injection region. During the recovery phase of the storm, when substorm activity diminished, precipitation due to density driven increases in the solar wind dynamic pressure (Pdyn) were identified. A number of increases in Pdyn were shown to drive sudden impulses (SIs) in the geomagnetic field. While many of these SIs appear coincident with CNA, SIs without CNA were also observed. During this period, the threshold of geomagnetic activity required for SC driven precipitation was exceeded. This implies that solar wind density driven SIs occurring during storm recovery can drive a different response in particle precipitation to typical SCs.


1986 ◽  
Vol 30 (1) ◽  
pp. 79-86
Author(s):  
Yu. V. Gotselyuk ◽  
M. S. Kazaryan ◽  
S. N. Kuznetsov ◽  
Karel Kudela ◽  
Ivan Kimák ◽  
...  

2010 ◽  
Vol 115 (A9) ◽  
pp. n/a-n/a ◽  
Author(s):  
Craig J. Rodger ◽  
Mark A. Clilverd ◽  
Neil R. Thomson ◽  
Rory J. Gamble ◽  
Annika Seppälä ◽  
...  

Atmosphere ◽  
2021 ◽  
Vol 12 (5) ◽  
pp. 573
Author(s):  
Tongxing Fu ◽  
Zhixu Wu ◽  
Peng Hu ◽  
Xin Zhang

In this paper, using the combined observations of the NOAA 16, LANL-01A, IMAGE satellites, VLF radio wave, and ground-based riometers, we study the fluctuation of lower ionosphere-associated precipitating energetic electrons during a geomagnetic storm on 8 November 2004. Associated with the substorm dispersion injection observed by the LANL-01A satellite, the riometers observed obvious enhancements of ionospheric absorption within the electron isotropic zone, which they attributed to the tail current sheet scattering (TCS) mechanism. Through observations of the NOAA 16 satellite, we found a sharp enhancement of the precipitating electron flux within the anisotropic zone, which entailed an obvious separation of energetic electron precipitation at high latitudes. This energetic electron precipitation within the anisotropic zone leads to the significant enhancement of electron density in the D region, thus resulting in the variations of VLF radio wave amplitudes, which propagate in the middle latitudes. Since the projection of the electron precipitation region within the anisotropic zone is at the inner edge of the plasmapause observed by the IMAGE EUV, the precipitation of energetic electrons should be attributed to the ELF hiss-ring current electron interaction. As a result, the energetic electron precipitations due to the tail current sheet scattering mechanism and wave-particle interaction in the inner magnetosphere were both observed and analyzed as they were associated with a substorm during a geomagnetic storm.


2011 ◽  
Vol 38 (20) ◽  
pp. n/a-n/a ◽  
Author(s):  
David A. Newnham ◽  
Patrick J. Espy ◽  
Mark A. Clilverd ◽  
Craig J. Rodger ◽  
Annika Seppälä ◽  
...  

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