Not exact matches
Data collected by ship and
model simulations suggest that increased Pacific Winter Water (PWW), driven by
circulation patterns and retreating sea ice in the summer season, is primarily responsible
for this OA expansion, according to Di Qi, the paper's lead author and a doctoral student of Liqi Chen, the lead PI in China.
Its number - crunching capabilities are used to study ship hydrodynamics and air turbulence, to probe industrial combustion turbines to create cleaner engines, and to understand global ocean
circulation, as well as
for earthquake
simulations and aircraft noise - reduction
modeling.
(Top left) Global annual mean radiative influences (W m — 2) of LGM climate change agents, generally feedbacks in glacial - interglacial cycles, but also specified in most Atmosphere - Ocean General
Circulation Model (AOGCM)
simulations for the LGM.
Model simulations of the thermohaline
circulation indicate that
for small perturbations, recovery can occur in a few decades.
As noted in that post, RealClimate defines the Atlantic Multidecadal Oscillation («AMO») as, «A multidecadal (50 - 80 year timescale) pattern of North Atlantic ocean - atmosphere variability whose existence has been argued
for based on statistical analyses of observational and proxy climate data, and coupled Atmosphere - Ocean General
Circulation Model («AOGCM»)
simulations.
An increased number of
simulations using EMICs or Atmosphere - Ocean General
Circulation Models (AOGCMs) that are the same as, or related to, the models used in simulations of the climates of the 20th and 21st centuries are available for these pe
Models (AOGCMs) that are the same as, or related to, the
models used in simulations of the climates of the 20th and 21st centuries are available for these pe
models used in
simulations of the climates of the 20th and 21st centuries are available
for these periods.
Here,
FOR values are derived from a General
Circulation Model by extracting OLR and SLE over areas in east - central Europe (at about 60 ° N) one hour after injecting appropriate CO2 concentration (adjustments to the atmospheric profile are thus excluded) to the Feb. 1 midnight
simulation.
Solomon et al. (2010) mentioned that NCAR Thermosphere - Ionosphere Electrodynamics General
Circulation Model (TIE - GCM) model simulations for ~ 97 — 600 km altitude showed, that the estimated change in total EUV energy input is approximately commensurate with the measured density ch
Model (TIE - GCM)
model simulations for ~ 97 — 600 km altitude showed, that the estimated change in total EUV energy input is approximately commensurate with the measured density ch
model simulations for ~ 97 — 600 km altitude showed, that the estimated change in total EUV energy input is approximately commensurate with the measured density change.
The time - independent linear response to these tropical anomalies is calculated
for extratropical basic states taken from reanalysis climatologies and also from the climatological states of Action de Recherche Petite Echelle Grande Echelle (ARPEGE) and Laboratoire de Mà © tà © orologie Dynamique (LMDZ) general
circulation model simulations.
The goal is to improve
model biases with regards to hydrographic measurements and
circulation constraints and use the improved
model for coupled ocean - atmosphere
simulations of preindustrial, historical and future climates.
We present a description of the ModelE2 version of the Goddard Institute
for Space Studies (GISS) General
Circulation Model (GCM) and the configurations used in the
simulations performed
for the...
Researchers project future climate using climate
models — computer - based numerical
simulations that use the equations
for fluid dynamics and energy transfer to represent atmospheric weather patterns and ocean
circulation.
Furthermore, the statistical methodology that is used to estimate the
model can successfully recover the values
for the transient climate response from temperature
simulations generated by the coupled atmosphere - ocean general
circulation models run
for CMIP (26).
A full description of the ModelE version of the Goddard Institute
for Space Studies (GISS) Atmospheric General
Circulation Model (GCM) and results are presented
for present - day climate
simulations (c. 1979).
Koch, D., D. Jacob, I. Tegen, D. Rind, and M. Chin, 1999: Tropospheric sulfur
simulation and sulfate direct radiative forcing in the Goddard Institute
for Space Studies general
circulation model.
Coupled climate
model simulations for a period of about 10,000 years would be probably needed to capture these kinds of
circulations (I am just speculating here).