A numerical simulation of an observed la
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C. Subbarao Maddukuri
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Article
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1982
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Springer
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English
โ 858 KB
A time-dependent, two-dimensional primitive-equation atmospheric boundary-layer model has been applied to the South shore of Lake Ontario, using data obtained by Estoque er cl/. (1976). The model has correctly predicted the times of onset, maximum intensity and disappearance of the lake breeze. Howe