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Assessing Climate Change Vulnerability of Breeding Birds in Arctic ...

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Section 1. IntroductionOf all places on the earth, climate change isoccurr<strong>in</strong>g most dramatically at the poles(Gillett et al. 2008). In the <strong>Arctic</strong>, airtemperature has <strong>in</strong>creased at almost twicethe global average rate <strong>in</strong> the past 100 years,accompanied by significantly alteredweather patterns, <strong>in</strong>creased glacial and polarpack ice melt, and sea level rise (IPCC2007). More specifically, <strong>in</strong> <strong>Arctic</strong> Alaskamean annual temperature is ris<strong>in</strong>g at a rate<strong>of</strong> 0.45 °C per decade (Data from M.Shulski reported <strong>in</strong> Mart<strong>in</strong> et al. 2009;Figure 1.1). Over the next 60 years, meanannual temperatures are expected to <strong>in</strong>creaseapproximately 5 °C (Figure 1.2) and to 7 °Cby the end <strong>of</strong> the century with most <strong>of</strong> thewarm<strong>in</strong>g occurr<strong>in</strong>g <strong>in</strong> w<strong>in</strong>ter (Mart<strong>in</strong> et al.2009). Annual precipitation is expected to<strong>in</strong>crease 20-40% over the next 60 years(Figure 1.3) although <strong>in</strong>creas<strong>in</strong>gtemperatures may lessen the effects <strong>of</strong><strong>in</strong>creased precipitation by driv<strong>in</strong>g an<strong>in</strong>crease <strong>in</strong> evapotranspiration rates (TWSSNAP http://www.snap.uaf.edu/data.php).While <strong>in</strong> some <strong>Arctic</strong> sites there is evidence<strong>of</strong> tundra dry<strong>in</strong>g, the pattern is spatiallyheterogeneous (e.g., Riordan et al. 2006). Itis uncerta<strong>in</strong> whether the future will br<strong>in</strong>g anet annual dry<strong>in</strong>g or moisten<strong>in</strong>g. Moreover,it is unclear how surface hydrology andgeomorphology changes will eitherexacerbate or compensate for shifts <strong>in</strong>atmospheric moisture (Mart<strong>in</strong> et al. 2009).Regionally, recent temperature and moisturechanges are lead<strong>in</strong>g to warm<strong>in</strong>g permafrost(Romanovsky et al. 2007), <strong>in</strong>creased coastalerosion (Jones et al. 2009), more frequentfires (Rac<strong>in</strong>e and Jandt 2008), and shrub<strong>in</strong>vasion (Tape et al. 2006), likely alter<strong>in</strong>ggeomorphology, hydrology, and habitatstructure (see Mart<strong>in</strong> et al. 2009 for athorough review).Key resources <strong>of</strong> concern <strong>in</strong> the <strong>Arctic</strong>are the vast productive wetlands <strong>in</strong> northernAlaska (particularly <strong>in</strong> the <strong>Arctic</strong> CoastalPla<strong>in</strong>) and the birds that migrate from allover the globe dur<strong>in</strong>g the brief summerseason to breed. Avian research <strong>in</strong> the regionpo<strong>in</strong>ts to the unique importance <strong>of</strong> largeparts <strong>of</strong> <strong>Arctic</strong> Alaska <strong>in</strong> harbor<strong>in</strong>g some <strong>of</strong>the most important avian breed<strong>in</strong>g grounds<strong>in</strong> the entire circumpolar <strong>Arctic</strong> (Andres etFigure 1.1. 50-year trend <strong>in</strong> mean annual temperature at seven sites on the North Slope (Source: M.Shulski <strong>in</strong> Mart<strong>in</strong> et al. 2009).3

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