Climate Warming - Global Summer Precipitation Scenario: 2100

Description

A simulation of the projected changes in June to August precipitation from the period 1975 to 1995 to the period 2080 to 2100 is shown on this map. On average, precipitation increases, but it is not evenly distributed geographically. There are marked regions of decreasing, as well as increasing precipitation, over both land and ocean. Annual average precipitation generally increases over northern continents, and particularly during the winter. Warmer surface temperature would speed up the hydrological cycle at least partially, resulting in faster evaporation and more precipitation. The results are based on climate change simulations made with the Coupled Global Climate Model developed by Environment Canada.

Resources

Name Format Description Link
Download the English JP2 File through HTTP Unknown https://ftp.geogratis.gc.ca/pub/nrcan_rncan/raster/atlas_6_ed/eng/65_climate_warming_global_summer_precipitation_scenario_2100.jp2
Download the English ZIP (PDF,JPG) file through HTTP ZIP https://ftp.geogratis.gc.ca/pub/nrcan_rncan/raster/atlas_6_ed/eng/65_climate_warming_global_summer_precipitation_scenario_2100.zip
Download the French JP2 File through HTTP Unknown https://ftp.geogratis.gc.ca/pub/nrcan_rncan/raster/atlas_6_ed/fra/65_rechauffement_climatique_scenario_precipitations_mondiales_estivales_2100.jp2
Download the French ZIP (PDF, JPG) File through HTTP ZIP https://ftp.geogratis.gc.ca/pub/nrcan_rncan/raster/atlas_6_ed/fra/65_rechauffement_climatique_scenario_precipitations_mondiales_estivales_2100.zip

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