Some characteristics of atmospheric gravity waves observed by radio-interferometry

Details Some characteristics of atmospheric gravity waves observed by radio-interferometry Some characteristics of atmospheric gravity waves observed by radio-interferometry

Jan 1996

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1996angeo..14...42m&link_type=abstract

Annales Geophysicae, vol. 14, Issue 1, pp.42-58

Physics

6

Scientific paper

Observations of atmospheric acoustic-gravity waves (AGWs) are considered through their effect on the horizontal gradient G of the slant total electron content (slant TEC), which can be directly obtained from two-dimensional radio-interferometric observations of cosmic radio-sources with the Nançay radioheligraph (2.2°E, 47.3°N). Azimuths of propagation can be deduced (modulo 180°). The total database amounts to about 800 h of observations at various elevations, local time and seasons. The main results are:

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