Wave structures in lower thermosphere density from satellite electrostatic triaxial accelerometer

Details Wave structures in lower thermosphere density from satellite electrostatic triaxial accelerometer Wave structures in lower thermosphere density from satellite electrostatic triaxial accelerometer

Aug 1995

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1995jgr...10014693f&link_type=abstract

Journal of Geophysical Research, Volume 100, Issue A8, p. 14693-14702

Physics

15

Meteorology And Atmospheric Dynamics: Thermospheric Dynamics, Meteorology And Atmospheric Dynamics: Waves And Tides

Scientific paper

High-resolution density data between 170 and 220 km from the SETA (Satellite Electrostatic Triaxial Accelerometer) Experiment during the summers of 1982 and 1983 are analyzed spectrally to investigate the nature of horizontal density structures ranging in scale from about 150 to 2500 km. The lower thermosphere is found to be frequently characterized by wavelike structures corresponding to peak-to-peak density variations of order 10-40%. Orbit-by-orbit spectral analyses of densities normalized to 200 km of altitude are performed, and these are combined to construct average periodgrams for magnetically quiet and active periods. Integration of these curves provides the relative percentage of total density variance attributable to various horizontal scales; for instance, 10% for λH<750 km and 70% for 1500<λH<2500 km. As geomagnetic activity increases from quiet (Kp<2) to active (Kp>4) levels, the spectral energy increases by a factor of 2 for wavelengths in the range 150 to 500 km and by a factor of 4 at longer wavelengths (1000-2500 km). In part the spectral energy enhancement at the longer wavelengths reflects mesoscale density variations unrelated to wave activity, but ``direct'' waves generated by auroral activity, which are known to travel long distances, probably also make important contributions at these wavelengths. The magnetic activity enhancement at shorter scales is also significant, especially at low latitudes, since waves with these horizontal wavelengths are not expected on theoretical grounds to propagate very far within the thermosphere away from an auroral source. Moreover, the shorter scale waves regularly occur during geomagnetically quiet times when an auroral source mechanism is unlikely.

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