Global thermosphere-ionosphere response to onset of 20 November 2003 magnetic storm

被引:116
作者
Crowley, G.
Hackert, C. L.
Meier, R. R.
Strickland, D. J.
Paxton, L. J.
Pi, X.
Mannucci, A.
Christensen, A. B.
Morrison, D.
Bust, G. S.
Roble, R. G.
Curtis, N.
Wene, G.
机构
[1] SW Res Inst, San Antonio, TX USA
[2] George Mason Univ, Sch Computat Sci, Fairfax, VA USA
[3] Computat Phys Inc, Springfield, VA USA
[4] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA
[5] CALTECH, Jet Prop Lab, Pasadena, CA USA
[6] Northrop Grumman Corp, Corp Headquarters, Los Angeles, CA USA
[7] Univ Texas San Antonio, Appl Res Lab, Austin, TX USA
[8] Natl Ctr Atmospher Res, High Altitude Observ, Boulder, CO 80307 USA
[9] Univ Texas San Antonio, San Antonio, TX 78285 USA
关键词
D O I
10.1029/2005JA011518
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
[ 1] There is great interest in understanding how the thermosphere-ionosphere system responds to geomagnetic storms. New insights are possible using the new generation of fully coupled three-dimensional models, together with extensive ionospheric databases. The period of postsolar maximum geomagnetic storms in October and November 2003 were some of the largest storms ever recorded. In this paper, we explore how the thermosphere-ionosphere system responded to the onset of the 20 November 2003 geomagnetic storm, using the NCAR TIMEGCM. The model simulates dramatic changes in the thermospheric equatorward winds, O/N-2, and corresponding ionospheric electron densities. The model is used as a framework to interpret an increase in the observed ionospheric total electron content, and F region electron density, in the European and North African sector, in terms of changes in the neutral gas. Corresponding compositional effects observed by the GUVI instrument on the TIMED satellite lend credence to the model results. We describe some of the important physical processes that will affect planning for the utilization of measurements from the Geospace investigations in NASA's Living With a Star Program. The study illustrates the value of measuring both the neutral and ionized gases, of obtaining quasi-global views from imaging instruments, and the synergy between satellite data, ground-based measurements, and models.
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页数:9
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