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The Oregon Climate Change Research Institute worked with the Climate Leadership Initiative at the University of Oregon to provide scenarios of future climate for the Lower Willamette Valley for their Climate Futures workshops. These workshops are held in the Portland Metro and the mid-Valley (Polk, Marion, Yamhill, Benton and Linn Counties) to educate citizens about the impacts of climate change in their areas. OCCRI provided maps of future anticipated changes in temperature and precipitation These products were created for the 2040 and 2080 time periods using a delta (change in temperature and precipitation) calculated for the Pacific Northwest from three General Circulation Models (CSIRO, HadCM, PCM) for the Pacific Northwest by Mote and Salathe (2009). This delta was applied to 800m PRISM data. Other products include:
OCCRI will be providing these products for future workshops in the Deschutes Basin. OCCRI will be providing a preliminary assessment of the risks and vulnerabilities climate change poses to the surface transportation infrastructure system in the Pacific Northwest and Alaska. OCCRI will:
OCCRI will also develop the base case for Climate Change in the Pacific Northwest and Alaska and characterize current conditions and trends. The information will be used to inform the decision making process regarding transportation infrastructure. This research will address:
OCCRI will collect and analyze trends and projected changes in climate, weather and geophysical variables. Using data from the North American Regional Climate Change Assessment Program (NARCCAP), OCCRI will assist the USGS and EPA in modeling the effects of climate change on estuaries in the Pacific Northwest. NARCCAP provides data parameters on a 50km grid, thus providing greatly improved resolution as compared to using General Circulation Model (GCM) parameters. OCCRI will also review the analysis of sea level rise in Mote et al. 2008 and consider the same factors for the Oregon Coast. This includes contributions from global sea level rise, local atmospheric dynamics and local vertical land movements. The estimates for central/southern Oregon will be adjusted by contributions from atmospheric dynamics and vertical land movements based on local estimates of tectonic movement (Verdonk 2006). |
