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21: NORTHWEST <br />the need to maintain streamflows and water quality for fish <br />and wildlife is balanced with human uses of water resources. <br />In highly managed rivers, release of deeper, colder water <br />from reservoirs could offer one of the few direct strategies to <br />lower water temperatures downstream.47 Actions to improve <br />stream habitat, including planting trees for shade, are being <br />tested. Some species may be able to change behavior or take <br />advantage of cold -water refuges.48 <br />Key Message 2: Coastal Vulnerabilities <br />In the coastal zone, the effects of sea level rise, erosion, inundation, threats to infrastructure <br />and habitat, and increasing ocean acidity collectively pose a major threat to the region. <br />With diverse landforms (such as beaches, rocky shorelines, <br />bluffs, and estuaries), coastal and marine ecosystems, and <br />human uses (such as rural communities, dense urban areas, <br />international ports, and transportation), the Northwest coast <br />will experience a wide range of climate impacts. <br />Description of Observed and Projected Changes <br />Global sea levels have risen about 8 inches since 1880 and <br />are projected to rise another 1 to 4 feet by 2100 (Ch. 2: <br />Our Changing Climate, Key Message 10). Many local and <br />regional factors can modify the global trend, including <br />vertical land movement, oceanic winds and circulation, <br />sediment compaction, subterranean fluid withdrawal (such as <br />groundwater and natural gas), and other geophysical factors <br />such as the gravitational effects of major ice sheets and glaciers <br />on regional ocean levels. <br />Much of the Northwest coastline is rising due to a geophysical <br />force known as "tectonic uplift," which raises the land surface. <br />Because of this, apparent sea level rise is less than the currently <br />observed global average. However, a major earthquake along <br />the Cascadia subduction zone, expected within the next few <br />hundred years, would immediately reverse centuries of uplift <br />and, based on historical evidence, increase relative sea level <br />40 inches or more.4958 On the other hand, some Puget Sound <br />as <br />Projected Relative Sea Level Rise <br />2020 2040 rya <br />Yew <br />locations are currently experiencing subsidence (where land is <br />sinking or settling) and could see the reverse effect, witnessing <br />immediate uplift during a major earthquake and lowered <br />relative sea levels."z <br />Taking into account many of these factors and considering <br />a wider range of emissions scenarios than are used in this <br />assessment (Appendix 5: Scenarios and Models), a recent <br />for the Latitude of Newport, Oregon <br />Figure 21.3. Projected relative sea level rise for the <br />latitude of Newport, Oregon (relative to the year 2000) <br />is based on a broader suite of emissions scenarios <br />(ranging from B1 to A1FI) and a more detailed and <br />regionally -focused calculation than those generally <br />used in this assessment (see Ch. 2: Our Changing <br />Climate).5Q The blue area shows the range of relative <br />sea level rise, and the black line shows the projection, <br />which incorporates global and regional effects of <br />24 warming oceans, melting land ice, and vertical land <br />movements.50 Given the difficulty of assigning likelihood <br />to any one possible trajectory of sea level rise at this <br />time, a reasonable risk assessment would consider <br />multiple scenarios within the full range of possible <br />outcomes shown, in conjunction with long- and short- <br />term compounding effects, such as El Nino -related <br />variability and storm surge. (Data from NRC 201250). <br />U.S. GLOBAL CHANGE RESEARCH PROGRAM 492 CLIMATE CHANGE IMPACTS IN THE UNITED STATES <br />