Meteorology for Air Pollution Control Engineers21

Meteorology for Air - at the troposphere-stratosphere boundary(Fig 5.5 n The stratosphere is practically isothermal and very stable against mixing

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2 n Next slide (Fig. 5.9) The tops of the clouds are not perfectly uniform, but they  are all at practically the same height, which corresponds  to the mixing height.
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4 n A stronger form of this mixing-height phenomenon exists 
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Unformatted text preview: at the troposphere-stratosphere boundary (Fig. 5.5) n The stratosphere is practically isothermal, and very stable against mixing from below....
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This note was uploaded on 10/14/2011 for the course CIVL CIVL345 taught by Professor Hsinchu during the Spring '11 term at SUNY College of Environmental Science and Forestry.

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Meteorology for Air - at the troposphere-stratosphere boundary(Fig 5.5 n The stratosphere is practically isothermal and very stable against mixing

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