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This Overview section

More detailed chapter from  "Foundation" report.

The National Assessment Overview and Foundation Reports were produced  by the National Assessment Synthesis Team, an advisory committee chartered under the Federal Advisory Committee Act, and were not subjected to OSTP's Information Quality Act Guidelines. The National Assessment was forwarded to the President and Congress in November 2000 for their consideration.

For background information on scenarios used in this assessment, see About Scenarios and Uncertainty and  Tools for Assessing Climate Change Impacts

By the 2090s, average summer temperatures are projected to rise by 7-8�F (4-4.5�C), while winter temperatures rise by 8-11�F (4.5-6�C). Projected annual average precipitation increases range from a few percent to 20% in the Hadley model, and from 20 to 50% in the Canadian model.

Water resources are already stressed by multiple growing demands. The projected warming and drier summers will likely increase summer water shortages, because there is less snowpack and because it melts earlier.

KEY ISSUES • Changes in Timing of Freshwater Resources • Added Stresses on Salmon • CO2 and Summer Drought Effects on Forests • Sea-level Rise Impacts on Coastal Erosion

The Pacific Northwest encompasses extensive forests, topography that creates abrupt changes in climate and ecosystems over short distances, and mountain and marine environments in close proximity. The Cascade Mountains divide the region climatically, ecologically, economically, and culturally. Three quarters of the region's population live west of the Cascades, concentrated in the metropolitan areas of Seattle and Portland, where the aerospace and computer industries have largely supplanted the traditional resource sectors of forestry, fishing, and agriculture. The Northwest provides a quarter of the nation's softwood lumber and plywood. The fertile lowlands of eastern Washington produce 60% of the nation's apples and large fractions of its other tree fruit.

The region has seen several decades of population and economic growth nearly twice the national rate, with population nearly doubling since 1970. The region's moderate climate, quality of life, and outdoor recreational opportunities contribute to its continuing attraction to newcomers. The same environmental attractions that draw people to the region are increasingly stressed by rapid development. Stresses arise from dam operation, forestry, and land-use conversion from natural ecosystems to metropolitan areas, intensively managed forests, agriculture, and grazing. The consequences include loss of old-growth forests, wetlands, and native grasslands; urban air pollution; extreme reduction of salmon runs; and increasing numbers of threatened and endangered species.

Observed Climate Trends

Over the 20th century, the region has grown warmer and wetter. Annual-average temperature has increased 1 to 3�F (0.5-1.5�C) over most of the region, with nearly equal warming in summer and winter. Annual precipitation has also increased across the region, by 10% on average, with increases reaching 30 to 40% in eastern Washington and Northern Idaho. The region's climate also shows significant recurrent patterns of year-to-year variability. Warm years tend to be relatively dry with low streamflow and light snowpack, while cool ones tend to be relatively wet with high streamflow and heavy snowpack. Though the differences in temperature and precipitation are small, they have clearly discernible effects on important regional resources. Warmer drier years tend to have summer water shortages, less abundant salmon, and increased probability of forest fires. These variations in the region's climate show clear correlations with two large-scale patterns of climate variation over the Pacific: the El Niño/Southern Oscillation (ENSO) on scales of a few years; and the more recently discovered Pacific Decadal Oscillation (PDO) on scales of a few decades. The observed effects of these patterns provide powerful illustrations of regional sensitivities to climate, but how they might interact with future climate change is not yet understood.

Scenarios of Future Climate

Model scenarios project regional warming in the 21st century to be much greater than observed during the 20th century, with average warming over the region of about 3�F (1.5�C) by the 2030s and 5�F (3�C) by the 2050s. By the 2090s, average summer temperatures are projected to rise by 7-8�F (4-4.5�C), while winter temperatures rise by 8-11�F (4.5-6�C). Through 2050, average precipitation is projected to increase, although some locations have small decreases. Precipitation increases would be concentrated in winter, with little change or a decrease in summer. Because of this seasonal pattern of wetter winters and drier summers, even the projections that show annual precipitation increasing, show water availability decreasing, especially in the Hadley model. By the 2090s, projected annual average precipitation increases range from a few percent to 20% in the Hadley model, and from 20 to 50% in the Canadian model.

Warming since 1900 in the Pacific Northwest ranges from 0 to 4�F.  By 2100, both models project warming near 5�F west of the Cascades, with much larger warming further east in the Canadian model. Precipitation has increased over most of the Pacific Northwest since 1900.  Both climate models project continued precipitation increases, with the largest increases in the southern part of the region.

Over the 21st century, both models project increases in annual average precipitation and in extreme precipitation events. As the graphs for both models show, the largest precipitation increases are projected to occur on days already receiving the most.

Changes in Timing of Freshwater Resources

Despite its reputation as a wet place, most of the Northwest receives less than 20 inches (0.5 meter) of precipitation a year, and dry summers make freshwater a limiting resource for many ecosystems and human activities. Water resources are already stressed by multiple growing demands. The projected warmer wetter winters will likely increase flooding in rainfed rivers, because there is more precipitation, and because more of it falls as rain. Projected year-round warming and drier summers will likely increase summer water shortages in both rainfed and snowfed rivers, including the Columbia, because there would be less snowpack and because it would melt earlier. In the Columbia, allocation conflicts are already acute, and the system is vulnerable to shortages.

Adaptations: Adapting to projected increases in summer shortages will likely require a combination of reducing demand, increasing supply, and reforming institutions to increase flexibility and regional problem-solving capacity. In the Colombia Basin, current infrastructure and institutions are inflexible and inadequate to deal with the projected scarcity.

Northwest forests are quite sensitive to climate variation because warm dry summers stress them directly, by limiting seedling establishment and summer photosynthesis, as well as indirectly, by creating conditions favorable to pests and fire. The extent, species mix, and productivity of Northwest forests are likely to change under projected 21st century climate change...

Severe storm surges and erosion are presently associated with El Niño events, which raise sea level for several months and change the direction of prevailing winds. Climate change is projected to bring similar shifts.

Added Stresses on Salmon

While non-climatic stresses on Northwest salmon presently overwhelm climatic ones, salmon abundances have shown a clear correlation with 20th century variations in climate from decade to decade. Climate models cannot yet project the most important oceanic conditions for salmon, but the likely effects on their freshwater habitat all appear unfavorable. Increased winter flooding, reduced summer and fall flows, and rising stream and estuary temperatures are all harmful for salmon. In addition, it is possible that earlier snowmelt and peak spring streamflow will deliver juveniles to the ocean before there is adequate food for them. Climate change is consequently very likely to hamper efforts to restore already depleted salmon stocks, and to stress presently healthy stocks.

Adaptations: It is possible that operational changes on managed rivers would reduce current stream warming and slow future warming, although such measures will very likely be overwhelmed by continued climate warming. Measures to reduce general stress on fish, such as changing dam operations to provide adequate late-summer streamflows, might possibly increase salmon's resilience to other stresses, including climate. It is very likely that maintaining such flows will become increasingly difficult, however, under the projected regional warming that will very likely shift peak streamflows to earlier in the year. Other options include maintaining the diversity of salmon by increasing preservation of their habitat, or removing existing dams and accepting reduced ability to manage summer shortages.

CO2 and Summer Drought Effects on Forests

Evergreen coniferous forests dominate the landscape of much of the Northwest. West of the Cascades, coniferous forests cover about 80% of the land, and include about half the world's temperate rainforest. Northwest forests have been profoundly altered by timber management and land-use conversion. These forests are quite sensitive to climate variation because warm dry summers stress them directly, by limiting seedling establishment and summer photosynthesis, as well as indirectly, by creating conditions favorable to pests and fire. The extent, species mix, and productivity of Northwest forests are likely to change under projected 21st century climate change, but the specifics of these changes are not known with confidence at present. They are very likely to depend on interactions between the timing and amount of precipitation, the seasonal water-storage capacity of forest soils, and changes in trees' water-use efficiency under elevated CO2. It is very likely that these factors will jointly determine the consequences of the likely increase in summer moisture stress, which will also depend on interactions with forest management practices, land-use conversion, and other pressures from development.

Adaptations: Options include planting species adapted to projected climate rather than present climate; managing forest density to reduce susceptibility to drought stress and fire risk; and using prescribed burning to reduce the risk of large, high-intensity fires. Increased capacity for long-term monitoring and planning would likely help with management. Reduced tree cutting, reduced road construction, and establishment of large buffers around streams are some of the ways to promote diversity of plant and animal species and the services provided by forest ecosystems (such as purifying air and water). Improved seasonal forecasts, and knowledge of the typical effects of ENSO and PDO, could possibly assist in decision making on timing and species of planting, and use and timing of prescribed burning.

Sea-level Rise Impacts on Coastal Erosion

Sea-level rise is likely to require substantial investments in order to avoid coastal inundation, especially in the low-lying communities of southern Puget Sound where coastal subsidence is occurring. Other likely effects include increases in winter landslides, and increased erosion on sandy stretches of the Pacific Coast. Severe storm surges and erosion are presently associated with El Niño events, which raise sea level for several months and change the direction of prevailing winds. Climate change is projected to bring similar shifts. Projected heavier winter rainfall is likely to increase soil saturation, landsliding, and winter flooding. All these changes would likely increase the danger to property and infrastructure on bluffs and beachfronts, and beside rivers.

Adaptations: The current coastal management system is not particularly adaptable, even to current climate variability and risks, and there is little inclination to restrict development in vulnerable locations. Adaptation strategies would involve conserving remaining natural coastal areas, placing less property at risk in low-lying or flood- or slide-prone areas, assigning more of the associated risk to property owners through insurance rates, and more effective transfer of climate change information to local governments, where most planning authority lies.