A theoretical investigation of the sea breeze

作者: M. A. Estoque

DOI: 10.1002/QJ.49708737203

关键词: Continuity equationHomogeneousMeteorologyGeologyType (model theory)Primitive equation modelTerrainSea breezeGeophysicsMotion (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.

参考文章(4)
H. R. Byers, H. E. Landsberg, H. Wexler, B. Haurwitz, A. F. Spilhaus, H. C. Willett, H. G. Houghton, Compendium of Meteorology American Meteorological Society. ,(1951) , 10.1007/978-1-940033-70-9
B. Haurwitz, Comments on the Sea-Breeze Circulation. Journal of Meteorology. ,vol. 4, pp. 1- 8 ,(1947) , 10.1175/1520-0469(1947)004<0001:COTSBC>2.0.CO;2
R. P. Pearce, The calculation of a sea-breeze circulation in terms of the differential heating across the coastline Quarterly Journal of the Royal Meteorological Society. ,vol. 81, pp. 351- 381 ,(1955) , 10.1002/QJ.49708134906
Raymond Wexler, Theory and Observations of Land and Sea Breezes Bulletin of the American Meteorological Society. ,vol. 27, pp. 272- 287 ,(1946) , 10.1175/1520-0477-27.6.272