Stability Properties of Large-Scale Atmospheric Disturbances
Stability Properties of Large-Scale Atmospheric Disturbances
复制标题
大规模大气扰动的稳定性特性
DOI：
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发表时间：
1951
期刊：
影响因子：
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通讯作者：
R. Fjørtoft
中科院分区：
文献类型：
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作者：
R. Fjørtoft
地球大气层的大范围运动基本上是从西向东的固体自转。在此基础上，叠加了相对运动中或多或少有序的纬向气流和气象学中常见的大尺度扰动。在这篇文章中，将讨论产生和维持这些扰动的原因，但不包括由于地球地形的不均匀而对大气施加的或多或少的永久性扰动。
The large-scale motion of the earth’s atmosphere is to the first approximation a solid rotation from west to east. Upon this are superimposed a more or less orderly zonal flow in the relative motion and the large-scale disturbances familiar in meteorology. In this article causes for the creation and maintenance of these disturbances will be discussed, excluding, however, the more or less permanent disturbances forced upon the atmosphere because of the earth’s topographic inhomogeneity.