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Qian Cao, Thomas H. Painter, William Ryan Currier, Jessica D. Lundquist, and Dennis P. Lettenmaier

Juan de Fuca to the north, and Puget Sound to the east (see Fig. 1 ). Elevations range from sea level to 2427 m at the top of Mt. Olympus in the interior of the Peninsula. Precipitation in this area is winter dominant, with over 80% of the annual total (on average over our domain) falling between October and April. The southwestern and western slopes of the Olympic Mountains are covered by dense temperate rain forest and receive plentiful winter precipitation due to orographic enhancement of

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