Latitudinal variability of the quasi-16-day wave in the middle atmosphere over Brazilian stations

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Abstract

A comparative study of the quasi-16-day wave (QSDW) in the middle atmosphere using meteor radar observations and reanalysis data from three Brazilian stations, Sao Joao do Cariri (7.4°S S, 36.5°S W) (CA), Cachoeira Paulista (22.7°S S, 45°S W) (CP), and Santa Maria (29.7°S S, 53.7°S W) (SM) has been carried out in the year 2005 to delineate its latitudinal variability characteristics. The broad spectral behavior around 16-day periodicity may indicate multiple modes of the concerned wave component. The wave amplitude shows a number of peaks over the year with the largest one in summer and winter in the case of mesosphere-lower thermosphere (MLT) and stratosphere, respectively. A potential coupling of the concerned wave with other short period planetary waves, especially at CA and CP is evinced. Although zonal propagation exhibits both eastward as well as westward waves there is a general preference of eastward waves at mid-latitude and westward waves at tropical latitudes. The prevailing westerly background wind in the middle atmosphere is conceived to favor the wave filtering of westward propagating Rossby waves at lower latitude.

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Guharay, A., Prado Batista, P., Robert Clemesha, B., Arlen Buriti, R., & Jorge Schuch, N. (2016). Latitudinal variability of the quasi-16-day wave in the middle atmosphere over Brazilian stations. Annales Geophysicae, 34(4), 411–419. https://doi.org/10.5194/angeo-34-411-2016

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