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Home > Research by the Foundation > Water Resources and Climate Change

 Overview

With uncertainty currently serving as the cornerstone of the climate change topic, many water resource managers are left to wonder what the future holds for their water supply. There is no single answer that will serve all utilities, as the complexity of global warming is as vast as the globe itself. Climate models, used to predict temperature and precipitation trends, point to varying impacts of climate change from region to region, with the potential effects on water supplies ranging from minimal to extreme. Water availability can be impacted by changes in precipitation, snowpack, runoff, increased evaporation and transpiration, and changes in demand. The challenge of water resource planning, therefore, will likely be greatly impacted if the value of historic precipitation and flow data diminishes in the wake of changes and variability in weather and temperature patterns.

As the earth warms, evaporation will increase. Higher levels of atmospheric moisture are expected to result in an average net increase in global precipitation, following the old adage of “what goes up must come down.”  This simple concept is quickly complicated by the fact that the greatest unknown factor is where the precipitation will fall. Unfortunately, while global models are mostly in agreement on anticipated regional temperature changes, models predicting expected changes in regional precipitation are not. Although there is disagreement among the models as to the exact locations where the greatest precipitation change will occur, most models indicate that the mid-latitude regions of the United States and much of Europe and Asia will experience the greatest changes (Climate Change and Water Resources: A Primer for Municipal Water Providers, order # 91120, research partner: National Center for Atmospheric Research). Some experts believe there may be fewer light and moderate rainfall events and more sporadic, heavy rainfall events, even in the areas that receive greater than historic precipitation. Likewise, areas with historic droughts may experience longer, more extreme drought events, and areas that have seen few droughts may find more frequent dry spells in their future.

IIn addition to changes in precipitation, the timing and intensity of snowpack runoff may also increase the likelihood of seasonal spring flooding events and decrease the amount of water available in rivers during the critical summer months. Water managers may find that existing infrastructure is less effective in managing greater extremes, from flooding to drought, and the capture and storage of water when it is available may have to be altered in areas where the greatest precipitation and temperature changes occur. Additionally, the potential for changes in seasonal flow will further stress sensitive ecosystems, increasing the tug of war between competing uses and reducing the amount of water available for human consumption during low flow.
 
 

 Foundation Resources That Can Help Utilities

Several resources are available from the Water Research Foundation to help water utilities make effective decisions related to water supply planning. Although only one of the following resources was developed in direct response to climate change challenges, all provide information that can assist water supply planners in the event that source-water quantity changes as a result of climate change.

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