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<p><strong>Abstract.</strong> A mathematical model of the global neutral wind system of the Earth's atmosphere, developed earlier in the Polar Geophysical Institute (PGI), is utilized to simulate the large-scale global circulation of the middle atmosphere for January conditions. The utilized model enables to calculate not only the horizontal components but also the vertical component of the neutral wind velocity by means of a numerical solution of a generalized Navier-Stokes equation fordoi:10.5194/adgeo-15-11-2008 fatcat:hf3lbkkyanelpfu73awzuxqd64