This corresponds in scope (not un-coincidentally) to the atmospheric
component of General Circulation Models (GCMs) coupled to (at least) a mixed - layer ocean.
Methods: Land surface models (LSMs) are an integral
component of the General Circulation Models (GCMs) and Earth System Models (ESMs).
This corresponds in scope (not un-coincidentally) to the atmospheric
component of General Circulation Models (GCMs) coupled to (at least) a mixed - layer ocean.
Not exact matches
O'Farrell, S.P., 1998: Investigation
of the dynamic sea ice
component of a coupled atmosphere sea - ice
general circulation model.
... A new sea - ice albedo parameterization scheme has been developed and implemented in ECHAM5
general circulation model, and includes important
components like albedo decay due to snow aging, ice thickness dependency and an explicit treatment
of melt pond albedo.
Abstract: «The patterns
of time / space changes in near - surface temperature due to the separate forcing
components are simulated with a coupled atmosphere — ocean
general circulation model»
The experiments were performed with ModelE2, a new version
of the NASA Goddard Institute for Space Sciences (GISS) coupled
general circulation model that includes three different versions for the atmospheric composition
components: a noninteractive version (NINT) with prescribed composition and a tuned aerosol indirect effect (AIE), the TCAD version with fully interactive aerosols, whole - atmosphere chemistry, and the tuned AIE, and the TCADI version which further includes a parameterized first indirect aerosol effect on clouds.
It became a basic
component of the UCLA
model for the
general circulation of the atmosphere.
Motivated by findings that major
components of so - called cloud «feedbacks» are best understood as rapid responses to CO2 forcing (Gregory and Webb in J Clim 21:58 — 71, 2008), the top
of atmosphere (TOA) radiative effects from forcing, and the subsequent responses to global surface temperature changes from all «atmospheric feedbacks» (water vapour, lapse rate, surface albedo, «surface temperature» and cloud) are examined in detail in a
General Circulation Model.
2, 3 The climate
model component is a two - dimensional (zonally averaged)
model that reproduces the behavior
of coupled atmosphere - ocean
general circulation models (AOGCMs).
We attempted to apply irrigation realistically in space and time to the land surface
component of a global atmosphere
general circulation model, the GISS ModelE, allowing the
model to compute explicitly the water and energy dynamics
of the land surface.