North American Regional Climate Change Assessment Program
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Timeseries Results: Maximum Temperature
 
Time series of precipitation are computed as the grid point average of monthly accumulation. The number of grid points within each region is determined by the map projection and the land-sea mask. Grid points over water are not included in the grid point average. The land-sea mask is generated for each model by using the land-sea mask of the CRU dataset. For each model grid point, the nearest CRU grid point is found and the surface type (land or water) of the CRU grid point is assigned to the model grid point.

 

 
Experiment 0.0
Experiment 0.1
Subarctic
60-70N, 135-95W
Northeast
40-50N, 85-70W
Northwest
38-55N, 122.5-115W
Southwest
20-35N, 115-110W
North Plains
40-55N, 102.5-90W
South Plains
30-40N, 102.5-90W
Southeast
32.5-40N, 90-80W
Canadian Maritime
42.5-55N, 70-50W
Canadian Prairie
42.5-55N, 120-100W
 
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