Therefore the agreement between
different General Circulation Models (GCMs) is correspondingly poorer.
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.
Using the adjoint of an ocean
general circulation model, I try to understand the local and remote processes that generate temperature anomalies in the Nordic Seas on
different timescales and their potential contribution to decadal climate predictability.
The factors and caveats that impact all of these
different recorders are also widely available in the literature, and more recently isotope - enabled
general circulation models have become more widely used in sync with observations (e.g., see Gavin Schmidt and others 2007 paper)
We employed two
different climate
model simulations: (1) the simulation of the NCAR CSM 1.4 coupled atmosphere - ocean General Circulation Model (GCM) analyzed by Ammann et al (2007) and (2) simulations of a simple Energy Balance Model (
model simulations: (1) the simulation of the NCAR CSM 1.4 coupled atmosphere - ocean
General Circulation Model (GCM) analyzed by Ammann et al (2007) and (2) simulations of a simple Energy Balance Model (
Model (GCM) analyzed by Ammann et al (2007) and (2) simulations of a simple Energy Balance
Model (
Model (EBM).
The factors and caveats that impact all of these
different recorders are also widely available in the literature, and more recently isotope - enabled
general circulation models have become more widely used in sync with observations (e.g., see Gavin Schmidt and others 2007 paper)
Comparing
different general circulation climate
models these researchers find it is actually only the (often - used) Hadley Centre
model that forces vegetation
models to a biome switch:
These results are obtained from 16 global
general circulation models downscaled with
different combinations of dynamical methods... http://dx.doi.org/10.1175/JCLI-D-12-00766.1
In the RCPs, the concentration of greenhouse gases is fixed at
different times in the future and the climate
model (or
general circulation model or GCM) uses those atmospheric concentrations to calculate future climate states.
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.
With all the many
different ways of calculating these numbers (empirically and from simple
models and
general circulation models), and
different results that have been obtained from these analyses, why hasn't this range and central value budged in over 3 decades?
Each atmospheric version is coupled to two
different ocean
general circulation models: the Russell ocean
model (GISS - E2 - R) and HYCOM (GISS - E2 - H).
Climate change was assessed by means of two Long Ashton Research Station - Weather Generator (LARS - WG) weather generators and all outputs from the available
general circulation models in the
Model for the Assessment of Greenhouse - gas Induced Climate Change - SCENario GENerator (MAGICC - SCENGEN) software, in combination with different emission scenarios at the regional scale, while the Providing Regional Climates for Impacts Studies (PRECIS) model has been used for projections at the local s
Model for the Assessment of Greenhouse - gas Induced Climate Change - SCENario GENerator (MAGICC - SCENGEN) software, in combination with
different emission scenarios at the regional scale, while the Providing Regional Climates for Impacts Studies (PRECIS)
model has been used for projections at the local s
model has been used for projections at the local scale.
The team looked at 99 water sub-basins using all 22
general circulation models used by the Intergovernmental Panel on Climate Change (IPCC) under three emissions scenarios and a number of
different indices for drought.
Three - dimensional (3D) planetary
general circulation models (GCMs) derived from the
models that we use to project 21st Century changes in Earth's climate can now be used to address outstanding questions about how Earth became and remained habitable despite wide swings in solar radiation, atmospheric chemistry, and other climate forcings; whether these
different eras of habitability manifest themselves in signals that might be detected from a great distance; whether and how planets such as Mars and Venus were habitable in the past; how common habitable exoplanets might be; and how we might best answer this question with future observations.