Geomagnetic disturbances and pulsations as a high-latitude response to considerable alternating IMF Variations during the magnetic storm recovery phase (Case study: May 30, 2003)

2015 ◽  
Vol 55 (6) ◽  
pp. 730-743 ◽  
Author(s):  
A. E. Levitin ◽  
N. G. Kleimenova ◽  
L. I. Gromova ◽  
E. E. Antonova ◽  
L. A. Dremukhina ◽  
...  
Keyword(s):  
Magnetic Storm ◽  
High Latitude ◽  
Recovery Phase ◽  
Geomagnetic Disturbances

Evolution of High-Latitude Geomagnetic Disturbances during the Magnetic Storm of July 22, 2009

2020 ◽  
Vol 60 (5) ◽  
pp. 547-558
Author(s):  
L. I. Gromova ◽  
N. G. Kleimenova ◽  
S. V. Gromov ◽  
L. M. Malysheva
Keyword(s):  
Magnetic Storm ◽  
High Latitude ◽  
Geomagnetic Disturbances

High-latitude geomagnetic disturbances during the initial phase of a recurrent magnetic storm (from February 27 to March 2, 2008)

2011 ◽  
Vol 51 (6) ◽  
pp. 730-740 ◽  
Author(s):  
N. G. Kleimenova ◽  
O. V. Kozyreva ◽  
J. Manninen ◽  
T. Raita ◽  
T. A. Kornilova ◽  
...  
Keyword(s):  
Magnetic Storm ◽  
High Latitude ◽  
Initial Phase ◽  
Geomagnetic Disturbances

High-latitude ionosphere convection and Birkeland current response for the 15 May 2005 magnetic storm recovery phase

2008 ◽  
Vol 113 (A3) ◽  
pp. n/a-n/a ◽  
Author(s):  
S. Eriksson ◽  
M. R. Hairston ◽  
F. J. Rich ◽  
H. Korth ◽  
Y. Zhang ◽  
...  
Keyword(s):  
Magnetic Storm ◽  
High Latitude ◽  
Recovery Phase ◽  
Current Response ◽  
High Latitude Ionosphere

scholarly journals The ionospheric storm studies: further development of the mapping technique

1996 ◽  
Vol 39 (4) ◽  
Author(s):  
I. Kutiev ◽  
T. Samardjiev ◽  
P. A. Bradley ◽  
M. I. Dick ◽  
L. R. Cander
Keyword(s):  
Magnetic Storm ◽  
Recovery Phase ◽  
Main Phase ◽  
Mapping Technique ◽  
Ionospheric Storm ◽  
Further Development

The technique of using instantaneous maps for ionospheric storm studies is further developed. Integral parameters are introduced characterizing the main features of each map. These parameters are the net volumes of ?f0F2, ?M(3000)F2and their gradients. The magnetic storm 1-2 March, 1982 was considered and it was found that before the storm commencement and in recovery phase the Net Gradient (NG) is directed steadily to the East, while in the main phase it turns southward. NG shows where the changes of the F-layer come from. The net volume of ?f0F2 (NF) correlates well with Dst and AE indices.

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