WEEKLY CLIMATE NEWS

DataStreme ECS WEEK ELEVEN: 19-23 April 2010


ITEMS OF INTEREST

CURRENT CLIMATE STATUS

CURRENT CLIMATE MONITORING

CLIMATE FORCING

CLIMATE MODELING

CLIMATE FORECASTS

PALEOCLIMATE RECONSTRUCTION

CLIMATE AND SOCIETY

COMPARATIVE PLANETOLOGY


Concept of the Week: Evolution of Climate Models

Climate scientists have been building increasingly sophisticated, mathematical climate models to serve two main purposes: test the sensitivity of the climate to altered conditions and simulate climate over time, either back into the past or forward into the future. The simplest, early type of climate model (zero dimensional) was the "energy balance model", which provides an average planetary temperature from incoming and outgoing radiation. A one-dimensional energy balance model determines the surface temperature from the energy balance at individual latitude belts.

More complex models involve the physical equations of motion (gas laws, thermodynamics and radiation interactions) subject to climate forcings, the boundary conditions of solar radiation, surface properties and atmospheric composition. As computers improved, models have included a three-dimensional oceanic circulation ("atmosphere-ocean coupling"), then interactions between the atmosphere, cryosphere and geosphere, with climate feedback mechanisms involving the exchanges of heat and water. Finally, models have been able to incorporate the improved knowledge of the biogeochemical processes. Climate models calculate variables such as temperature at individual points within the three-dimensional grid of cells across the Earth's surface and vertically through the atmosphere, ocean, ice and land. A tradeoff exists between the number of grid points (the spatial resolution) and the number of numerical computations. Time and space accuracy costs increased computational time and expense.

The development of numerical weather prediction models during the 1960s and 1970s spurred the development of General Circulation Models (GCMs) for climate. One of the early atmospheric GCMs was developed at Princeton University's Geophysical Fluid Dynamics Laboratory (GFDL). By the 1990s, comprehensive climate models were being perfected with three-dimensional oceanic circulation. Ultimately, the term GCM could be used to refer to a Global Climate Model that represents the major climate system components (atmosphere, ocean, land surface and polar ice) and their interactions. The Community Climate Model at the National Center for Atmospheric Research is one of the most comprehensive climate models currently available. This model has been used to determine the future temperature response for several scenarios concerning the release of greenhouse gases through the 21st century as proposed by the IPCC reports.

Concept of the Week: Questions

(Place your responses on the Chapter Progress Response Form provided in the Study Guide.)

  1. General circulation models are generally [(less), (more)] sophisticated than energy balance models.
  2. Increasing the spatial resolution of a global climate model causes the computational time to [(increase),(decrease),(remain the same)].

Historical Events:


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Prepared by Edward J. Hopkins, Ph.D., email hopkins@meteor.wisc.edu
© Copyright, 2010, The American Meteorological Society.