The baroclinity formed by the horizontal temperature gradient is the main reason for the formation of the wind shear.

水平温度梯度形成较强的斜压性是形成边界层风切变的主要原因。

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The baroclinity formed by the horizontal temperature gradient is the main reason for the formation of the wind shear.

水平温度梯度形成较强的斜压性是形成边界层风切变的主要原因。

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