Identification
Title
A numerical investigation of boundary layer quasi-equilibrium
Abstract
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.
Resource type
document
Resource locator
Unique resource identifier
code
http://n2t.net/ark:/85065/d7rn3928
codeSpace
Dataset language
eng
Spatial reference system
code identifying the spatial reference system
Classification of spatial data and services
Topic category
geoscientificInformation
Keywords
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Text
originating controlled vocabulary
title
Resource Typereference date
date type
publication
effective date
2016-01-01T00:00:00Z
Geographic location
West bounding longitude
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Temporal reference
Temporal extent
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Dataset reference date
date type
publication
effective date
2015-01-28T00:00:00Z
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Copyright 2015 American Geophysical Union.
Limitations on public access
None
Responsible organisations
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contact position
OpenSky Support
organisation name
UCAR/NCAR - Library
full postal address
PO Box 3000
Boulder
80307-3000
email address
opensky@ucar.edu
web address
http://opensky.ucar.edu/
name:
homepage
responsible party role
pointOfContact
Metadata on metadata
Metadata point of contact
contact position
OpenSky Support
organisation name
UCAR/NCAR - Library
full postal address
PO Box 3000
Boulder
80307-3000
email address
opensky@ucar.edu
web address
http://opensky.ucar.edu/
name:
homepage
responsible party role
pointOfContact
Metadata date
2023-08-18T19:03:02.932838
Metadata language
eng; USA