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首页> 外文期刊>Acta Meteorologica Sinica >The influence of stratification on frontogenesis caused by geostrophic adjustment
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The influence of stratification on frontogenesis caused by geostrophic adjustment

机译:地层调整对分层对前生的影响

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摘要

A uniform, inviscid, incompressible fluid in a two-dimensional plane(x, z)is considered. three principles: conservation of potential vorticity, conservation of absolute momentum, and conservation of mass are used for this study. If the initial mass field and the initial wind field do not satisfy geostrophic balance, then through geostrophic adjustment under suitable conditions, the frontogenesis will finally occur. Our work points out that initial density distribution greatly influences the frontal features. If the stratification in cold air is the same as that in warm air, two frontogeneses will occur at top and bottom boundaries respectively.
机译:考虑在二维平面(x,z)中均匀,无粘性,不可压缩的流体。本研究使用三个原理:保持潜在的涡度,保持绝对动量和保持质量。如果初始质量场和初始风场不满足地转平衡,则通过在适当条件下进行地转调整,最终会发生前生。我们的工作指出,初始密度分布会极大影响正面特征。如果在冷空气中的分层与在热空气中的分层相同,则将在顶部和底部边界分别出现两个前生。

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