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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 />

14

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