Precipitation extremes and their potential future changes were predicted using six - member
ensembles of general circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 5 (CMIP5).
Not exact matches
In an
ensemble of fully coupled atmosphere - ocean
general circulation model (AOGCM) simulations
of the late Paleocene and early Eocene, we identify such a
circulation - driven enhanced intermediate - water warming.
Methods: In these experiments, the research team conducted large
ensembles of simulations with two state -
of - the - art atmospheric
general circulation models by abruptly switching the sea - surface temperature warming on from January 1st to focus on the wintertime
circulation adjustment.
Climate change projections were based on an
ensemble of four
General Circulation Models (UKMO HadCM3, MPIM ECHAM5, CSIRO MK3.5 and GFDL CM2.1), downscaled to 10 minutes [32], considering three emissions scenarios (B2, A1B and A2) for 1975 (mean 1961 — 1990), 2050 (mean 2041 — 2060) and 2090 (mean 2081 — 2100).
Rowlands (2012) write, «Here we present results from a multi-thousand-member perturbed - physics
ensemble of transient coupled atmosphere — ocean
general circulation model simulations.
The
ensemble and seasonal forecast systems use a coupled atmosphere - ocean
model, which includes a simulation
of the
general circulation of the ocean and the associated coupled feedback processes that exist.
Here we present results from a multi-thousand-member perturbed - physics
ensemble of transient coupled atmosphere — ocean
general circulation model simulations.
When heavy rainfall probabilities were next investigated in
ensembles of two atmospheric
general circulation models, run with and without anthropogenically - induced sea surface temperature changes, results were
model - dependent.