Vertical density and temperature structure over northern Europe

Document ID: 61

Philbrick, C. Russell1
Grossmann, K. U.2
Hennig, R.2
Lange, G.2
Krankowsky, D.3
Offermann, D.2
Schmidlin, F. J.4
von Zahn, Ulf5

1 USAF, Geophysics Laboratory, Hanscom AFB, Bedford, MA, U.S.A.
2 University of Wuppertal, Wuppertal, F.R.G.
3 Max-Planck-Institut für Kernphysik, Heidelberg, F.R.G.
4 NASA Goddard Space Flight Center, Wallops Flight Facility, Wallops Island, VA, U.S.A.
5 University of Bonn, Bonn, F.R.G.
 

Abstract

During the Energy Budget Campaign, several profiles of the density and temperature of the upper atmosphere were obtained. The measurements were made using rocket-borne instrumentation launched from ESRANGE, Sweden and Andoya Rocket Range, Norway during November and December, 1980. The techniques included meteorological temperature sondes, passive falling spheres, accelerometer instrumented falling spheres, density gauges, mass spectrometers and infrared emission experiments. The instruments provided data within the altitude range from 20 km to 150 km. The measurements were made during periods which have been grouped into three categories by level of geomagnetic activity. Analysis has been made to compare the results and to examine the oscillations and fluctuations in the vertical profiles for scales ranging between hundreds of meters and tens of kilometers. Most of the features observed fit qualitatively within the range expected for internal gravity waves. The geomagnetic storm conditions may be associated with enhanced wave activity and heating observed in the lower thermosphere.

 

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Citation:        "Vertical density and temperature structure over northern Europe", Philbrick, C. R., K. U. Grossmann, R. Hennig, G. Lange, D. Krankowsky, D. Offermann, F. J. Schmidlin, U. von Zahn, Advances in Space Research, Vol. 2, No. 10, COSPAR (Committee on Space Research), 1983, pp. 121 - 124, CCC: 0273—1177/83/100121-04