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AGU: Journal of Geophysical Research, Space Physics

 

Keywords

  • composition
  • ionosphere
  • winds

Index Terms

  • Ionosphere: Ionospheric disturbances
  • Atmospheric Composition and Structure: Thermosphere: composition and chemistry
  • Ionosphere: Electric fields
  • Ionosphere: Midlatitude ionosphere
  • Ionosphere: Ionosphere/atmosphere interactions
Abstract
Cited By (14)
 

Abstract

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

G. Crowley

Southwest Research Institute, San Antonio, Texas, USA

C. L. Hackert

Southwest Research Institute, San Antonio, Texas, USA

R. R. Meier

School of Computational Sciences, George Mason University, Fairfax, Virginia, USA

D. J. Strickland

Computational Physics Inc., Springfield, Virginia, USA

L. J. Paxton

Johns Hopkins University, Applied Physics Laboratory, Laurel, Maryland, USA

X. Pi

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

A. Mannucci

Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA

A. B. Christensen

Northrop Grumman Corporation, Corporate Headquarters, Los Angeles, California, USA

D. Morrison

Johns Hopkins University, Applied Physics Laboratory, Laurel, Maryland, USA

G. S. Bust

Applied Research Laboratory, University of Texas of Austin, Austin, Texas, USA

R. G. Roble

National Center for Atmospheric Research, High Altitude Observatory, Boulder, Colorado, USA

N. Curtis

Southwest Research Institute, San Antonio, Texas, USA

G. Wene

University of Texas at San Antonio, San Antonio, Texas, USA

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/N2, 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.

Received 3 November 2005; accepted 17 July 2006; published 18 October 2006.

Citation: Crowley, G., et al. (2006), Global thermosphere-ionosphere response to onset of 20 November 2003 magnetic storm, J. Geophys. Res., 111, A10S18, doi:10.1029/2005JA011518.

Cited By

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