Conserving Freshwater and Coastal Resources in a Changing Climate
Conserving Freshwater and Coastal Resources in a Changing Climate
Conserving Freshwater and Coastal Resources in a Changing Climate
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Table 2. <strong>Freshwater</strong> Wetl<strong>and</strong>s: Impacts of <strong>Climate</strong> Changes<br />
<strong>Climate</strong> Driven Change<br />
Anticipated Effects on<br />
<strong>Freshwater</strong> Wetl<strong>and</strong><br />
Potential Response of<br />
Wetl<strong>and</strong><br />
• Lower summer water<br />
levels<br />
• More frequent<br />
droughts<br />
• Increase of isolation <strong>and</strong><br />
fragmentation with<strong>in</strong> wetl<strong>and</strong>s<br />
• Dry<strong>in</strong>g of bogs<br />
• Loss of habitat, migration corridors;<br />
Organisms dependent on water for<br />
mobility may be threatened<br />
• Amphibian <strong>and</strong> fish reproduction fail<br />
more often <strong>in</strong> drier years<br />
• Loss of hydrologic connections to<br />
riparian zones <strong>and</strong> groundwater systems<br />
Decrease <strong>in</strong> precipitation<br />
fall<strong>in</strong>g as snow, result<strong>in</strong>g <strong>in</strong> a<br />
meager snow pack<br />
Annual spr<strong>in</strong>g flood may occur earlier<br />
<strong>and</strong> be weaker than current patterns<br />
Vegetation shift as the less flood-tolerant<br />
species out-compete those which need<br />
predictable <strong>in</strong>undation<br />
Warmer Temperatures<br />
• Increase <strong>in</strong> evaporation<br />
• Decrease <strong>in</strong> dissolved oxygen <strong>in</strong><br />
the water<br />
• Exacerbates the already low<br />
summer water levels<br />
• Survival of species compromised<br />
due to lack of oxygen<br />
• Species at southern extent of their<br />
range may become ext<strong>in</strong>ct<br />
Increased w<strong>in</strong>ter storm<br />
<strong>in</strong>tensity<br />
• Wetl<strong>and</strong>s more vulnerable to<br />
<strong>in</strong>tense w<strong>in</strong>d <strong>and</strong> ra<strong>in</strong> activity<br />
• Increase <strong>in</strong> storm-water run-off<br />
carry<strong>in</strong>g pollutants, sediment <strong>and</strong><br />
excess nutrients<br />
• Wetl<strong>and</strong>s may be compromised<br />
or destroyed<br />
• Increased pollution levels <strong>in</strong><br />
surround<strong>in</strong>g water sources as wetl<strong>and</strong>s<br />
ability to filter is compromised<br />
Loss of Wetl<strong>and</strong> Filter<strong>in</strong>g Capacity<br />
The comb<strong>in</strong>ation of more frequent droughts <strong>and</strong> heavy<br />
storms is likely to reduce the capacity of wetl<strong>and</strong>s to<br />
filter sediment <strong>and</strong> pollutants. Less filter<strong>in</strong>g will yield<br />
<strong>in</strong>creased levels of sediments <strong>and</strong> tox<strong>in</strong>s <strong>in</strong> the surround<strong>in</strong>g<br />
waters. Additional pollution could enter the<br />
ecosystem as water levels drop <strong>in</strong> rivers <strong>and</strong> lakes <strong>and</strong> a<br />
greater amount of soil is exposed to the air. Increases <strong>in</strong><br />
oxygen concentration with<strong>in</strong> the soil, especially when<br />
coupled with acid deposition, may trigger the release of<br />
metals such as cadmium, copper, lead <strong>and</strong> z<strong>in</strong>c <strong>in</strong>to the<br />
environment. These additional load<strong>in</strong>gs could amplify<br />
problems <strong>in</strong> areas where there are already an elevated<br />
prevalence of heavy metal contam<strong>in</strong>ation such as near<br />
<strong>in</strong>dustrial discharges (Kl<strong>in</strong>g et al., 2003).<br />
The level of overall nutrients be<strong>in</strong>g delivered <strong>in</strong>to<br />
the wetl<strong>and</strong>s may decrease <strong>in</strong> summer as the freshwater<br />
<strong>Conserv<strong>in</strong>g</strong> <strong>Freshwater</strong> <strong>and</strong> <strong>Coastal</strong> <strong>Resources</strong> <strong>in</strong> a Chang<strong>in</strong>g <strong>Climate</strong><br />
sources, which typically provide the majority of nutrients,<br />
are compromised by drought conditions (Kl<strong>in</strong>g et<br />
al., 2003). Despite an <strong>in</strong>crease <strong>in</strong> decomposition rates<br />
from <strong>in</strong>creas<strong>in</strong>g temperatures, the warmer air <strong>and</strong> water<br />
comb<strong>in</strong>ed with fluctuat<strong>in</strong>g water levels are likely to<br />
reduce the wetl<strong>and</strong>’s capacity to assimilate nutrients<br />
<strong>and</strong> other materials transported <strong>in</strong> stormwater runoff<br />
(Kl<strong>in</strong>g et al., 2003).<br />
Altered Flood<strong>in</strong>g of Floodpla<strong>in</strong> Forests<br />
A key source of water for floodpla<strong>in</strong> forests <strong>and</strong> wetl<strong>and</strong>s<br />
is the flood regime of the river, stream or lake along<br />
which they exist (Sorenson et al., 1998). Water levels<br />
fluctuate <strong>in</strong> time with the flood<strong>in</strong>g, evaporation <strong>and</strong> soil<br />
saturation (Moore et al., 1997; Department of Ecology,<br />
2007). Floodpla<strong>in</strong>s also receive water directly from<br />
ra<strong>in</strong>, groundwater <strong>and</strong> surface run-off but are adapted<br />
to the cycles of <strong>in</strong>undation <strong>and</strong> disturbance associated<br />
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