作者: M. A. Estoque
关键词: Continuity equation 、 Homogeneous 、 Meteorology 、 Geology 、 Type (model theory) 、 Primitive equation model 、 Terrain 、 Sea breeze 、 Geophysics 、 Motion (geometry) 、 Atmospheric Science
摘要: A primitive equation model is formulated and integrated numerically to study the sea breeze. The formulation an extension of atmospheric boundary-layer previously developed for a homogeneous terrain. External gravity-wave type solutions are suppressed by modelling assumption involving continuity. results integration showing evolution breeze under conditions no large-scale synoptic motion presented.