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ider a vertical column of the atmosphere at 43°N (f=104 s'). The geostrophic wind is 10 ms from the south at 900 hPa, and 10 ms from the west at 700 hPa. Calculate the mean horizontal temperature gradients in the layer. Compute the rate of advective temperature change in the layer.

ider a vertical column of the atmosphere at 43°N (f=104 s'). The geostrophic wind is 10 ms from the south at 900 hPa, and 10 ms from the west at 700 hPa. Calculate the mean horizontal temperature gradients in the layer. Compute the rate of advective temperature change in the layer.

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2. Consider a vertical column of the atmosphere at 43°N (f-104 s!). The geostrophic wind is 10 ms from the south at 900 hPa, and 10 ms from the west at 700 hPa. Calculate the mean horizontal temperature gradients in the layer. Compute the rate of advective temperature change in the layer.
Transcribed Image Text:2. Consider a vertical column of the atmosphere at 43°N (f-104 s!). The geostrophic wind is 10 ms from the south at 900 hPa, and 10 ms from the west at 700 hPa. Calculate the mean horizontal temperature gradients in the layer. Compute the rate of advective temperature change in the layer.
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