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In this thesis, we present a mathematical model that represents internal gravity waves and convection generated by a thermal forcing in the atmosphere. The goal is to investigate the mechanisms by which deep heating and convection in the lower atmosphere generate internal gravity waves. We consider a two-dimensional two-layer model ofdoi:10.22215/etd/2014-10291 fatcat:2ryqf45ofnfflji36wtiggfpv4