Throughout the world, efforts are under way to restore watersheds, but restoration planning rarely accounts for future climate change. Using a series of linked models of climate, land cover, hydrology, and salmon population dynamics, we investigated the impacts of climate change on the effectiveness of proposed habitat restoration efforts designed to recover depleted Chinook salmon populations in a Pacific Northwest river basin. Model results indicate a large negative impact of climate change on freshwater salmon habitat. Habitat restoration and protection can help to mitigate these effects and may allow populations to increase in the face of climate change. The habitat deterioration associated with climate change will, however, make salmon recovery targets much more difficult to attain. Because the negative impacts of climate change in this basin are projected to be most pronounced in relatively pristine, high-elevation streams where little restoration is possible, climate change and habitat restoration together are likely to cause a spatial shift in salmon abundance. River basins that span the current snow line appear especially vulnerable to climate change, and salmon recovery plans that enhance lower-elevation habitats are likely to be more successful over the next 50 years than those that target the higher-elevation basins likely to experience the greatest snow-rain transition.Chinook salmon ͉ hydrologic model ͉ population model ͉ Snohomish River ͉ stream flow O ver the past decade, billions of dollars have been spent on the restoration of aquatic habitats throughout the United States (1). In the northwestern U.S., aquatic habitat restoration has been driven largely by the Endangered Species Act, under which several species of Pacific salmon have been listed. The listings have led to the development of salmon recovery plans for watersheds throughout the region. Long-term freshwater habitat protection and restoration projects are central to all plans. Planners rely heavily on fish habitat models to evaluate the potential effectiveness of proposed restoration strategies, and numerous models have been developed to predict restoration effects. In almost all cases, these models assume stationary future climate conditions when assessing how restoration will affect fish abundance and productivity. Given the increasing certainty that climate change is accelerating, models that ignore the potential effects of future climate may generate misleading predictions of the relative benefits of different recovery strategies.The northwestern U.S. has warmed by between 0.7 and 0.9°C during the 20th century. Since 1950, average annual air temperatures at the majority of meteorological stations in the region have risen by Ϸ0.25°C/decade (2), and climate models predict another 1.5-3.2°C increase by the middle of the 21st century (3). Higher air temperatures are likely to increase water temperatures, which could be harmful to salmon during the spawning, incubation, and rearing stages of their life cycle (4). Warmer temperatures a...