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Conserving Freshwater and Coastal Resources in a Changing Climate

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Tim<strong>in</strong>g of Seasonal Phenomena:<br />

• The Northeast will experience the start of<br />

summer (def<strong>in</strong>ed as grow<strong>in</strong>g degree days – those<br />

above 65°F) 6-11 days earlier, <strong>and</strong> it will extend<br />

10-16 days longer <strong>in</strong>to the fall by mid-century.<br />

The end of the century is projected to see a<br />

summer season that arrives 9-21 days earlier, <strong>and</strong><br />

that extends 12 days to 3 weeks longer <strong>in</strong>to the<br />

fall (UCS 2006).<br />

• The grow<strong>in</strong>g season <strong>in</strong> the Northeast is predicted<br />

to be 2-4 weeks earlier by the middle of this<br />

century <strong>and</strong> 4-6 weeks longer by the end of the<br />

century (UCS 2006). The grow<strong>in</strong>g season <strong>in</strong> the<br />

Great Lakes region is expected to be 4 to 9 weeks<br />

longer (Kl<strong>in</strong>g, 2003).<br />

• The length of the Northeast’s snow season is<br />

expected to decl<strong>in</strong>e by 25-50% (UCS 2006).<br />

Weather Patterns<br />

<strong>Climate</strong> models predict changes <strong>in</strong> weather patterns<br />

throughout the eastern United States. The summer <strong>and</strong><br />

fall months will be hotter <strong>and</strong> drier, with periods of extreme<br />

drought. This will cause evaporation rates to <strong>in</strong>crease,<br />

effectively lower<strong>in</strong>g the water levels throughout<br />

wetl<strong>and</strong>s <strong>and</strong> the entire watershed (Moore et al., 1997).<br />

In addition, the ground may become drier which decreases<br />

its ability to absorb ra<strong>in</strong> when it does fall, which<br />

then contributes to erosion (M. Kl<strong>in</strong>e, personal communication,<br />

April 13, 2007). Thus, dur<strong>in</strong>g the w<strong>in</strong>ter <strong>and</strong><br />

spr<strong>in</strong>g, when heavy precipitation events are predicted,<br />

the ground will be less able to absorb the <strong>in</strong>flux of ra<strong>in</strong>water,<br />

<strong>and</strong> there will be large <strong>in</strong>creases <strong>in</strong> the amount of<br />

stormwater runoff, carry<strong>in</strong>g with it higher quantities of<br />

sediment, excess nutrients, <strong>and</strong> pollutants (Kl<strong>in</strong>g et al.,<br />

2003; Najjar et al., 2000).<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 />

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