{"refrec":{"BRefID":8908,"RR":"<b>Gallée, H.; Schayes, G.; Berger, A.</b> (1993). Development of a 3-dimensional meso-gamma primitive equations model: katabatic winds simulation in the area of Terra Nova Bay, Antarctica, <b><i>in</i></b>: Caschetto, S. (Ed.) <i>Belgian scientific research programme on Antarctica: scientific results of phase II (10/1988-05/1992): 3. Glaciology and climatology.</i> pp. II/03/1-36","BEntID":8908,"PublicFlag":1,"CheckedFlag":0,"wosflag":null,"vabbflag":null,"RefStringPartII":", <b><i>in</i></b>: Caschetto, S. (Ed.) <i>Belgian scientific research programme on Antarctica: scientific results of phase II (10/1988-05/1992): 3. Glaciology and climatology. Belgian scientific research programme on Antarctica,</i> : pp. II/03/1-36","DocTypID":17,"DocType":"Book chapters","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Gallée, H.; Schayes, G.; Berger, A.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Gallée, H.; Schayes, G.; Berger, A.","Englishabstract":"The spatial evolution of Antarctic katabatic winds in the area of Terra Nova Bay is examined using the three-dimensional version of the UCL/MAR <i> Modèle Atmosphérique Régional</i> mesoscale primitive equation model. The ability of the model to replicate classical linear and nonlinear mountain waves simulations is verified. Then, a three-dimensional experiment is performed using the terrain configuration of Terra Nova (Ross Sea coastal zone). Because of computational requirements, the discretization is chosen to be 5 km. Results are in good agreement with availahle ohservations and previous modeling work. 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