Not exact matches
Le Treut, H., Z.X. Li, and M. Forichon, 1994:
Sensitivity of the LMD
general circulation model to greenhouse forcing associated with two different cloud water parametrizations.
«Seasonal Cycle Experiments on Climate
Sensitivity Due to a Doubling
of CO2 with an Atmospheric
General Circulation Model Coupled to a Simple Mixed Layer Ocean
Model.»
«The
Sensitivity of Monsoon Climates to Orbital Parameterization Changes for 9000 Years BP: Experiments with the NCAR
General Circulation Model.»
The three successive IPCC reports (1991 [2], 1996, and 2001 [3]-RRB- concentrated therefore, in addition to estimates
of equilibrium
sensitivity, on estimates
of climate change over the 21st century, based on several scenarios
of CO2 increase over this time interval, and using up to 18
general circulation models (GCMs) in the fourth IPCC Assessment Report (AR4)[4].
Computer simulations
of the climate, referred to as «
general circulation models» (GCMs), can be used to assess the
sensitivity of climate to changes that might result from increased greenhouse gases.
13.2.1 Incremental Scenarios for
Sensitivity Studies 13.2.2 Analogue Scenarios 13.2.2.1 Spatial analogues 13.2.2.2 Temporal analogues 13.2.3 Scenarios Based on Outputs from Climate
Models 13.2.3.1 Scenarios from General Circulation Models 13.2.3.2 Scenarios from simple climate models 13.2.4 Other Types of Sce
Models 13.2.3.1 Scenarios from
General Circulation Models 13.2.3.2 Scenarios from simple climate models 13.2.4 Other Types of Sce
Models 13.2.3.2 Scenarios from simple climate
models 13.2.4 Other Types of Sce
models 13.2.4 Other Types
of Scenarios
Lo, 1997:
Sensitivity of northern hemisphere air temperatures and snow expansion to North Pacific sea surface temperatures in the Goddard Institute for Space Studies
general circulation model.
The
sensitivity of NPP to climate change is especially uncertain because it depends on changing soil water availability, which varies significantly between
General Circulation Models (GCMs), with some models suggesting major drying and reduced productivity in tropical ecosystems (Cox et al.,
Models (GCMs), with some
models suggesting major drying and reduced productivity in tropical ecosystems (Cox et al.,
models suggesting major drying and reduced productivity in tropical ecosystems (Cox et al., 2004).
Contrary to Schlesinger's result, the majority
of state -
of - the - art four - dimensional «
general circulation models» (GCMs)- the kind used in the Trenberth and Fasullo study - estimate the climate
sensitivity is closer to 3 degrees C.