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