1998 Annual Report
Biological and Environmental Research

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


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/


 INDEX  NEXT >>