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National Winter Precipitation Scenario: 2050

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Abstract

A simulation of projected changes in winter (December to February) precipitation from the period 1961 to 1990 to the period 2040 to 2060 for Canadian lands is shown here. In general, precipitation would increase as the century progresses and the climate warms. Projected precipitation changes are not evenly distributed geographically or seasonally. Precipitation is projected to decrease slightly for some higher latitude regions. 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.

Projected Change

This map shows the projected change in winter (December to February) precipitation from the reference period 1961 to 1990 to the middle (2040 to 2060) of the current century for Canadian land areas. These changes are the response simulated in the Canadian Centre for Climate Modelling and Analysis (CCCma) global climate model to projected increases in atmospheric greenhouse gas concentrations and sulfate aerosol loadings associated with human activity. Precipitation changes are expressed as percentages to indicate that a given change in precipitation amount is more important in a region of low average precipitation than in a region of high average precipitation.

In general, precipitation increases as the century progresses and the climate warms. Projected precipitation changes are not evenly distributed geographically nor seasonally. There are regions with decreases of precipitation as well as those with increases. Precipitation is projected to decrease slightly for some higher latitude regions.

The following animation is created to show the projected change from year 1995 to 2070 in mean annual precipitations relative to 1961 to 1990 average.

Explanations

The hydrological cycle speeds up at least partially because the warmer surface temperatures cause increased evaporation into the atmosphere which then becomes available for precipitation. The marked regions of both increasing and decreasing precipitation are associated with shifts in the broad patterns of atmospheric circu­lation under climate warming.

Data Source

The results are based on climate change simulations made with the Coupled Global Climate Model (CGCM2) developed at the Canadian Centre for Climate Modelling and Analysis of Environment Canada. The projected changes in greenhouse gases concentrations and aerosol loadings are based on the IS92a scenario developed in conjunction with the Intergovernmental Panel on Climate Change to portray one of several possible futures. The output of the model is produced on a grid of 3.75 degrees in latitude and longitude. This represents a grid square of approximately 400 kilometres by 300 kilometres at Canadian latitudes. For forestry and other applications, the Canadian Forest Service of National Resources Canada has derived the changes in climate based on the simulation output with reference to the 1961 to 1990 normals, and interpolated the data over Canada to finer resolution using a multi-step methodology.

The digital data for this map can be downloaded here.

Caution in Interpreting the Map

The aim of global climate models is to simulate past, current, and future large-scale climate based on the physical principles governing the climate system. The Canadian Centre for Climate Modelling and Analysis model is reasonably successful in reproducing the current climate and the climate change observed over the past century. Nevertheless, future climate scenario results must be treated with caution and this is especially the case when results are viewed at smaller local scales. Regional climate models are one approach to "downscaling" the large-scale results from global climate models to more local scales. These models are under active development in Canada and elsewhere.

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Date modified: 2004-04-05 Top of Page Important Notices