Abstract
Longitudinal dependences of stratospheric GW (gravity wave) fluctuations and lower ionospheric irregularities (sporadic E) at mid latitudes are studied by means of radio occultation data of the GPS/MET satellite mission. The zonal average of temperature variance of GW fluctuations with vertical scales less than 7 km at northern mid latitudes is observed to be similar to that at southern mid latitudes, but there is a significant interhemispheric difference in the longitudinal dependence of GW fluctuations. The GPS/MET data at northern mid latitudes show a rapid change of the gravity wave distribution from 25 to 35 km height, resulting in a broad maximum of temperature variance located over Atlantic and Eurasia. We only find in the wave distribution at h=25 km some weak traces of possible orographic effects. On the other hand, the distribution of GW fluctuations at southern mid latitudes has a strong and sharp maximum over Andes which is obviously due to orographic wave generation by interaction of surface wind with the Andean mountain ridge. This observation of the new GPS radio occultation technique is in agreement with previous measurements of spaceborne microwave and infrared limb sounders. The amplitude of the average wave field increases with height over Andes, while the amplitude maximum moves westward, against the prevailing wind. The temperature fluctuations have an apparent, dominant vertical wave length of around 6 km. In situ measurements by a balloon-borne rawinsonde at Ushuaia, Argentina (54.7°S, 68.1°W) are compared to a simultaneous GPS/MET temperature profile. The balloon observations of temperature and horizontal wind are interpreted by a large amplitude mountain wave propagating to the upper stratosphere. Finally, the GPS/MET experiment indicates enhanced sporadic E in the lower ionosphere over Southern Andes. We assume that these plasma irregularities are generated by enhanced, upward wave flux due to the possible orographic effect of Andes.
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