Mean upper contour patterns of the northern hemisphere — the thermal-synoptic view-point

Mean upper contour patterns of the northern hemisphere — the thermal-synoptic view-point
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北半球的平均上等线模式——热天气观点

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发表时间:
1951
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通讯作者:
R. Sutcliffe
R. Sutcliffe
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文献类型:
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作者:
R. Sutcliffe

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研究了 1 月和 7 月北半球平均 500 mb 等值线模式和 1,000-500 mb 厚度模式。考虑了 Bolin (1950) 提倡的地形动力假说。主要基于斜压天气过程改变的陆地和海洋的直接热效应的热天气解释被认为是令人满意的。
The mean 500 mb contour patterns and 1,000-500 mb thickness patterns for the northern hemisphere in January and July are examined. The orographic-dynamical hypothesis advocated by Bolin (1950) is considered. A thermal-synoptic explanation, resting mainly on the direct thermal effects of land and sea modified by baroclinic synoptic processes, is regarded as satisfactory.