Surface fluxes and vertical profiles in the radix layer
The bottom two kilometers of the earth's atmosphere, called the atmospheric boundary layer (ABL) , can be vigorously mixed by convective circulations when the underlying surface is warmer than the air. Mixing can be so complete that the mean wind speed, MUL, and potential temperature, θUL, i...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/9990 |