Physically-Based Global Downscaling Climate Change Projections for a Full Century

Journal Article · Fri Apr 15 04:00:00 EDT 2005 · Journal of Physics: Conference Series, 16:343-347

DOI:https://doi.org/10.1088/1742-6596/16/1/047· OSTI ID:965612

Ghan, Steven J; Shippert, Timothy R

A global atmosphere/land model with an embedded subgrid orography scheme is used to simulate the period 1977-2100 using ocean surface conditions and radiative constituent concentrations for a climate change scenario. Climate variables simulated for multiple elevation classes are mapping according to a high-resolution elevation dataset in ten regions with complex terrain. Analysis of changes in the simulated climate leads to the following conclusions. Changes in precipitation vary widely, with precipitation increasing more with increasing altitude in some region, decreasing more with altitude in others, and changing little in still others. In some regions the sign of the precipitation change depends on surface elevation. Changes in surface air temperature are rather uniform, with at most a two-fold difference between the largest and smallest changes within a region; in most cases the warming increases with altitude. Changes in snow water are highly dependent on altitude. Absolute changes usually increase with altitude, while relative changes decrease. In places where snow accumulates, an artificial upper bound on snow water limits the sensitivity of snow water to climate change considerably. The simulated impact of climate change on regional mean snow water varies widely, with little impact in regions in which the upper bound on snow water is the dominant snow water sink, moderate impact in regions with a mixture of seasonal and permanent snow, and profound impacts on regions with little permanent snow.

• Research Organization: Pacific Northwest National Laboratory (PNNL), Richland, WA (US)
• Sponsoring Organization: USDOE
• DOE Contract Number: AC05-76RL01830
• OSTI ID: 965612
• Report Number(s): PNNL-SA-44905; KP1206000
• Journal Information: Journal of Physics: Conference Series, 16:343-347, Journal Name: Journal of Physics: Conference Series, 16:343-347
• Country of Publication: United States
• Language: English