Satellite in-situ electron density observations of the storm enhanced density and the polar Tongue of Ionization on the noon meridional plane in the F region during the 20 November 2003 magnetic storm

Satellite in-situ electron density observations of the storm enhanced density 2 and the polar Tongue of Ionization on the noon meridional plane in the F 3 region during the  The first report on sa...

[1]  E. Sutton,et al.  Occurrence Locations, Dipole Tilt Angle Effects, and Plasma Cloud Drift Paths of Polar Cap Neutral Density Anomalies , 2018 .

[2]  E. Thomas,et al.  Ionospheric F-region response to the 26 September 2011 geomagnetic storm in the Antarctica American and Australian sectors , 2017 .

[3]  A. Komjathy,et al.  Revisiting Ionosphere‐Thermosphere Responses to Solar Wind Driving in Superstorms of November 2003 and 2004 , 2017 .

[4]  Wenbin Wang,et al.  Relative importance of horizontal and vertical transports to the formation of ionospheric storm‐enhanced density and polar tongue of ionization , 2016 .

[5]  Takuji Nakamura,et al.  Formation of polar ionospheric tongue of ionization during minor geomagnetic disturbed conditions , 2015 .

[6]  B. Lovell,et al.  Storm‐enhanced plasma density and polar tongue of ionization development during the 15 May 2005 superstorm , 2015 .

[7]  Liu Hui,et al.  Energetics characteristics of the super magnetic storm on November 20, 2003 based on 3D global MHD simulation , 2014 .

[8]  A. Komjathy,et al.  Interplanetary magnetic field By control of prompt total electron content increases during superstorms , 2014 .

[9]  Biqiang Zhao,et al.  A study on the nighttime midlatitude ionospheric trough , 2011 .

[10]  H. Lühr,et al.  IRI‐2007 model overestimates electron density during the 23/24 solar minimum , 2010 .

[11]  J. Retterer,et al.  Solar wind drivers for low-latitude ionosphere models during geomagnetic storms , 2010 .

[12]  S. Skone,et al.  Monitoring storm-enhanced density using IGS reference station data , 2009 .

[13]  P. Alken,et al.  Penetration characteristics of the interplanetary electric field to the daytime equatorial ionosphere , 2008 .

[14]  B. Tsurutani,et al.  Interplanetary conditions leading to superintense geomagnetic storms (Dst ≤ −250 nT) during solar cycle 23 , 2008 .

[15]  Anthony J. Mannucci,et al.  Superposed epoch analysis of the dayside ionospheric response to four intense geomagnetic storms , 2008 .

[16]  S. Watanabe,et al.  Solar activity dependence of the electron density in the equatorial anomaly regions observed by CHAMP , 2007 .

[17]  B. Reinisch,et al.  Comparison of CHAMP and Digisonde plasma frequencies at Jicamarca, Peru , 2007 .

[18]  Mark B. Moldwin,et al.  Unusual topside ionospheric density response to the November 2003 superstorm , 2005 .

[19]  W. Rideout,et al.  Multiradar observations of the polar tongue of ionization , 2005 .

[20]  N. Tsyganenko,et al.  Modeling the dynamics of the inner magnetosphere during strong geomagnetic storms , 2005 .

[21]  M. Buonsanto Ionospheric Storms — A Review , 1999 .

[22]  Ludger Scherliess,et al.  Empirical models of storm time equatorial zonal electric fields , 1997 .

[23]  Nikolai A. Tsyganenko,et al.  Modeling the Earth's magnetospheric magnetic field confined within a realistic magnetopause , 1995 .

[24]  L. Scherliess,et al.  Time dependent response of equatorial ionospheric electric fields to magnetospheric disturbances , 1995 .

[25]  M. Buonsanto Millstone Hill incoherent scatter F region observations during the disturbances of June 1991 , 1995 .

[26]  J. Foster Storm time plasma transport at middle and high latitudes , 1993 .

[27]  Lou‐Chuang Lee,et al.  Energy coupling function and solar wind‐magnetosphere dynamo , 1979 .

[28]  J. Evans The causes of storm-time increases of the F-layer at mid-latitudes , 1973 .

[29]  J. Klobuchar,et al.  Simultaneous storm-time increases of the ionospheric total electron content and the geomagnetic field in the dusk sector , 1971 .

[30]  C. Reigber,et al.  First champ mission results for gravity, magnetic and atmospheric studies , 2003 .

[31]  D. Anderson Modeling the midlatitude F-region ionospheric storm using east-west drift and a meridional wind , 1976 .