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2014/07/16 Council Agenda Packet
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2014/07/16 Council Agenda Packet
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Council Agenda Packet
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7/16/2014
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21: NORTHWEST <br />evaluation calculated projected sea level rise and ranges for <br />the years 2030, 2050, and 2100 (relative to 2000) based on <br />latitude for Washington, Oregon, and California (see Figure <br />21.3).50 In addition to long-term climate -driven changes in <br />sea level projected for the Northwest, shorter -term El Nino <br />conditions can increase regional sea level by about 4 to 12 <br />inches for periods of many months.5o53 <br />Northwest coastal waters, some of the most productive on the <br />West Coast,54 have highly variable physical and ecological con- <br />ditions as a result of seasonal and year-to-year changes in up - <br />welling of deeper marine water that make longer -term changes <br />difficult to detect. Coastal sea surface temperatures have in- <br />creased55 and summertime fog has declined between 1900 <br />and the early 2000s, both of which could be consequences of <br />weaker upwelling winds.56 Projected changes include increas- <br />ing but highly variable acidity,57'58'59 increasing surface water <br />temperature (2.2°F from the period 1970 to 1999 to the period <br />2030 to 2059),60 and possibly changing storminess.61 Climate <br />models show inconsistent projections for the future of North- <br />west coastal upwelling.12'62 <br />Consequences and Likelihoods of Changes <br />In Washington and Oregon, more than 140,000 acres of <br />coastal lands lie within 3.3 feet in elevation of high tide.63 As <br />sea levels continue to rise, these areas will be inundated more <br />frequently. Many coastal wetlands, tidal flats, and beaches will <br />probably decline in quality and extent as a result of sea level <br />rise, particularly where habitats cannot shift inland because <br />of topographical limitations or physical barriers resulting from <br />human development. Species such as shorebirds and forage <br />fish (small fish eaten by larger fish, birds, or mammals) would <br />be harmed, and coastal infrastructure and communities would <br />be at greater risk from coastal storms.64 <br />Ocean acidification threatens culturally and commercially <br />significant marine species directly affected by changes in ocean <br />chemistry (such as oysters) and those affected by changes in <br />the marine food web (such as Pacific salmon65). Northwest <br />coastal waters are among the most acidified worldwide, <br />especially in spring and summer with coastal upwelling5859'66 <br />combined with local factors in estuaries.57'58 <br />Increasing coastal water temperatures and changing ecological <br />conditions may alter the ranges, types, and abundances of <br />marine species.67'68 Recent warm periods in the coastal ocean, <br />for example, saw the arrival of subtropical and offshore marine <br />species from zooplankton to top predators such as striped <br />marlin, tuna, and yellowtail more common to the Baja area.69 <br />Warmer water in regional estuaries (such as Puget Sound) <br />may contribute to a higher incidence of harmful blooms of <br />algae linked to paralytic shellfish poisoning,7° and may result <br />in adverse economic impacts from beach closures affecting <br />recreational harvesting of shellfish such as razor clams.'' <br />Toxicity of some harmful algae appears to be increased by <br />acidification.'2 <br />Rising Sea Levels <br />and Changing Flood Risks in Seattle <br />Figure 21.4. Areas of Seattle projected by Seattle Public <br />Utilities to be below sea level during high tide (Mean Higher <br />High Water) and therefore at risk of flooding or inundation <br />are shaded in blue under three levels of sea level rise,'$ <br />assuming no adaptation. (High [50 inches] and medium <br />[13 inches] levels are within the range projected for the <br />Northwest by 2100; the highest level [88 inches] includes the <br />compounding effect of storm surge, derived from the highest <br />observed historical tide in Seattle79). Unconnected inland <br />areas shown to be below sea level may not be inundated, but <br />could experience problems due to areas of standing water <br />caused by a rise in the water table and drainage pipes backed <br />up with seawater. (Figure source: Seattle Public Utilities80). <br />Many human uses of the coast — for living, working, and <br />recreating — will also be negatively affected by the physical <br />and ecological consequences of climate change. Erosion, <br />inundation, and flooding will threaten public and private <br />property along the coast; infrastructure, including wastewater <br />treatment plants;7'73 stormwater outfalls;74'75 ferry terminals;76 <br />and coastal road and rail transportation, especially in <br />Puget Sound.77 Municipalities •from Seattle74 and Olympia,75 <br />Washington, to Neskowin, Oregon, have mapped risks from <br />the combined effects of sea level rise and other factors. <br />U.S. GLOBAL CHANGE RESEARCH PROGRAM 493 CLIMATE CHANGE IMPACTS IN THE UNITED STATES <br />
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