Of these, radiative and radiative -
convective equilibrium models have received great attention..
The Planck response of 1.2 K for GCMs comes from one - dimensional radiative
convective equilibrium models (1DRCM) that assume the fixed lapse rate of 6.5 K / km (FLRA) and use the mathematical method of Cess (1976), equation (3).
Not exact matches
For simplicity, assume all solar heating at the surface (so that the lapse rate is (1 - dimensional climate
model, radiative
convective equilibrium) positive or approaching zero but never negative) unless otherwise stated:
They had built the first completely correct radiative -
convective implementation of the standard
model applied to Earth, and used it to calculate a +2 C
equilibrium warming for doubling CO2, including the water vapour feedback, assuming constant relative humidity.
Even a simple ocean
model usually has a number of slightly different
equilibria actually, due to shifts in the location of
convective activity (by a few grid boxes - I'm not talking here about a big reorganisation of the circulation).
Through the use of a Venus climate
model that couples atmospheric radiative -
convective equilibrium with surface processes, we show that it is likely that Venus» climate is at or near a state of unstable
equilibrium.
In our «rotating radiative
convective equilibrium» simulations, a realistic
model is simplified by removing land surfaces and spherical geometry, and by assuming that the underlying ocean temperatures are spatially uniform, providing a relatively simple system in which to study the formation and mature structure of hurricanes.
From its heritage from 1D radiative -
convective models of the earth's atmosphere, the IPCC AR4 WGI Section 2.2 describes the concept of determining the change in
equilibrium surface temperature from radiative forcing (RF):
The calculations by Kuang 2010 in which a dynamic
model of radiative -
convective equilibrium is perturbed systematically with different heat (and moisture) sources suggests that this is the path of least resistance for a convecting atmosphere, but that there are other possibilities as well — I need to understand this paper better.