By Meghan M. Dalton, Philip Mote, Amy K. Snover
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Extra resources for Climate Change in the Northwest: Implications for Our Landscapes, Waters, and Communities
Change in summer averaged daily maximum 8-hr ozone mixing ratios (ppbv) between a future case (2045–2054) and base case (1990–1999) based on future climate from a model forced with the continued growth emissions scenario (SRES-A2). Changes in ground-level ozone are due to global and local emissions, changes in environmental conditions and urbanization, and increasing summer temperatures. Adapted from Chen et al. (2009). ȱ ȱ ȱ Ěȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱ ȱȱȱ ȱȱȱȱ ǰȱ¢ȱȱ ȱȱȱCryptosporidiumȱǯȱȱȱȱȱȱ¢ȱĴȱin ȱ ȱȱȱ¢ȱŘŖŖŖȱ¢ȱȱȱȱȱȱǯ ȱȱȱȱȱȱȱȱ¢ȱęȱȱȱȱ poisoning in humans.
Executive Summary £ȱȱȱȱ¢ȱǯȱȱ ȱȱ¢ȱȱ ¢ȱȱȱȱȱȱȱȱ ǰȱȱȱ ȱ ęȱȱȱ Ĵȱǯȱȱȱȱ ȱȱȱǰȱȱȱ¢ȱȱȱȱ ȱȱ ȱȱȱȱ2 concentrations. Climate change in rangeland systems may alter pressure from invasive species leading to degradation.
7. Areas of recent fire and insect disturbance in the Northwest. outbreaks is expected to increase, particularly in high-elevation forests. Certain forest ǰȱȱȱ ȱȱȱȱȬęǰȱȱȱ¡ȱȱȱȱȱ future. 3) ȱȬȱȱȱ¢ȱȱȱĚȱ¢ȱǰȱȱ drought can cause host trees to be more vulnerable to insects, leading to higher tree mor¢ǯȱȱ¢ȱȱȱȱȱȱȱȱȱȱȱ¡ȱ ȱȱ ȱȱ ȱȱȱ ǰȱ¢ȱȱȬȱȱ ȱȱ¢¢ȱȱȱȱȱȱǯȱȱȱĚȱȱȱȱ survival of forest pathogens, but the climate-disease relationship is unclear for many ȱȱȱȱȬȱǯȱ ȱȱȱȱ increased spring precipitation in the Oregon Coast Range have contributed to an inȱȱ¢ȱȱȱȱ ȱȱȱȱȬęǰȱ ȱȱȱ to have a greater impact in the future.