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Future Precipitation and Storm Changes

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Precipitation Changes | Storm Changes

Precipitation Changes

According to the IPCC, an increase in the average global temperature is very likely to lead to changes in precipitation and atmospheric moisture because of changes in atmospheric circulation and increases in evaporation and water vapor.

Two maps of the globe showing projected changes in precipitation under a climate change scenario. The top map shows changes for December, January, and February; the bottom map shows changes for June, July, and August. In general, the high northern latitudes are projected to become much wetter (20 percent or more) in winter, while large areas of the tropics become dryer in both winter and summer. The maps also indicate areas (in white) where fewer than two-thirds of the climate models agreed on how precipitation will change. Stippled areas reveal where more than 90 percent of the models agreed. Image is from IPCC WG1 AR-4, 2007.

Climate models suggest (IPCC, 2007):

However, regional precipitation projections from climate models must be considered with caution since they demonstrate limited skill at small spatial scales.

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Storm Changes

Mid-latitude storm tracks are projected to shift toward the poles, with increased intensity in some areas but reduced frequency. Tropical storms and hurricanes are likely to become more intense, produce stronger peak winds, and produce increased rainfall over some areas due to warming sea surface temperatures (which can energize these storms) (IPCC, 2007). The relationship between sea surface temperatures and the frequency of tropical storms is less clear.  There is currently no scientific consensus on how future climate change is likely to affect the frequency of tropical storms in any part of the world where they occur. (WMO, 2006)

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