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AGU: Geophysical Research Letters

 

Keywords

  • thermosphere density
  • solar minimum

Index Terms

  • Atmospheric Composition and Structure: Thermosphere: composition and chemistry
  • Atmospheric Composition and Structure: Pressure, density, and temperature
  • Atmospheric Composition and Structure: Thermosphere: energy deposition
  • Solar Physics, Astrophysics, and Astronomy: Solar activity cycle
  • Space Weather: Satellite drag

Abstract

GEOPHYSICAL RESEARCH LETTERS, VOL. 37, L12102, 5 PP., 2010
doi:10.1029/2010GL043671

Record-low thermospheric density during the 2008 solar minimum

J. T. Emmert

Space Science Division, Naval Research Laboratory, Washington, D. C., USA

J. L. Lean

Space Science Division, Naval Research Laboratory, Washington, D. C., USA

J. M. Picone

Department of Physics and Astronomy, George Mason University, Fairfax, Virginia, USA

We use global-average thermospheric total mass density, derived from the drag effect on the orbits of many space objects, to study the behavior of the thermosphere during the prolonged minimum in solar activity between cycles 23 and 24. During 2007–2009 thermospheric densities at a fiducial altitude of 400 km were the lowest observed in the 43-year database, and were anomalously low, by 10–30%, compared with climatologically expected levels. The density anomalies appear to have commenced before 2006, well before the cycle 23/24 minimum, and are larger than expected from enhanced thermospheric cooling by increasing concentrations of CO2. The height dependence of the mass density anomalies suggests that they are attributable to a combination of lower-than-expected exospheric temperature (−14 K) and reductions in the number density of atomic oxygen (−12%) and other species (−3%) near the base of the diffusive portion of the thermosphere.

Received 19 April 2010; accepted 19 May 2010; published 19 June 2010.

Citation: Emmert, J. T., J. L. Lean, and J. M. Picone (2010), Record-low thermospheric density during the 2008 solar minimum, Geophys. Res. Lett., 37, L12102, doi:10.1029/2010GL043671.

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