Coupled Parallel Climate Model (PCM) Applications
to Climate Change
Warren M. Washington and Gerald A. Meehl, National Center for
Atmospheric Research
Albert Semtner, Naval Postgraduate School
John Weatherly, Cold Regions Research and Engineering Laboratory
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Research Objectives
To conduct simulations of climate change with new generation high-resolution
climate models.
Computational Approach
The Parallel Climate Model (PCM) is a coupled climate model that
executes on the Cray T3E computer. The atmospheric component is
the National Center for Atmospheric Research (NCAR) Community
Climate Model; the ocean component is the Parallel Ocean Program
with a resolution of 32 levels and 2/3 degree horizontal grid;
and the sea ice component is the Naval Postgraduate School model
using a resolution of 27 km. The components are interfaced by
a flux coupler that passes the energy, moisture, and momentum
fluxes between components.
Accomplishments
Over the past year we were able to obtain a climate simulation
for the 1990s. We will use this control experiment for future
climate change scenarios with different forcings such as increasing
greenhouse gases and the effects of sulfate aerosols. This model
has higher-resolution ocean and sea ice components than are used
in previous coupled climate model simulations; thus we can see
much more realistic eddy structures in the ocean that are closer
to the observed patterns.
Significance
Because of an observed warming of the earth's climate that is
probably caused by increased greenhouse gases, the Department
of Energy is very interested in making better estimates of possible
impacts on future states of climate. This requires, in part, better
models of the climate system with improved resolution that provides
regional impacts. |
This image (click on it for a larger version)
depicts the sea surface temperature (Celsius scale) from a coupled simulation
with the DOE Parallel Climate Model. Note the Gulf Stream meander pattern and
the cooler tropical Pacific and Atlantic surface temperatures caused by
upwelling of cold water. Also depicted is the cold water under the Arctic and
East Greenland sea ice. (Graphic by Gary Strand, NCAR.)
Publications
W. M. Washington and J. W. Weatherly, "Simulations
with a climate model with high-resolution ocean and sea ice,"
in Polar Processes and Global Climate: Draft Summary Report
from the Conference on Polar Processes and Global Climate, WMO/ICSU/IOC
World Climate Research Programme (WCRP) (International ACYSYS
Project Office, Oslo, Norway, 1997), pp. 250-252.
http://www.cgd.ucar.edu/ccr/pcm/
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