A numerical investigation of boundary layer quasi-equilibrium

Despite the large energy input from surface evaporation, the moist static energy (MSE) of the tropical boundary layer remains relatively constant on large spatial and temporal scales due to lifting of vapor by cloudy updrafts and the addition of dry air from the layers above. Arakawa and Schubert (1974) suggested that drying is due mainly to clear-air turbulent entrainment between cloudy updrafts, while Raymond (1995) described drying due mainly to convective downdrafts. We used cloud-resolving numerical simulations to investigate the transport of MSE into the boundary layer and found turbulent entrainment between clouds to be the dominant process.

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Copyright 2015 American Geophysical Union.


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Author Thayer-Calder, Kate
Randall, David
Publisher UCAR/NCAR - Library
Publication Date 2015-01-28T00:00:00
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Topic Category geoscientificInformation
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Metadata Date 2023-08-18T19:03:02.932838
Metadata Record Identifier edu.ucar.opensky::articles:16553
Metadata Language eng; USA
Suggested Citation Thayer-Calder, Kate, Randall, David. (2015). A numerical investigation of boundary layer quasi-equilibrium. UCAR/NCAR - Library. http://n2t.net/ark:/85065/d7rn3928. Accessed 10 February 2025.

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