State Climate Summaries for the United States 2022. NOAA Technical Report NESDIS 150.

Kunkel, K.E., R. Frankson, J. Runkle, S.M. Champion, L.E. Stevens, D.R. Easterling, B.C. Stewart, A. McCarrick, and C.R. Lemery (Eds.)

WASHINGTON

Washington’s location in the heart of the middle latitudes exposes it to frequent storm systems associated with the mid-latitude jet stream. Due to the physical barrier of the Cascade Mountains, the climate differs greatly in the western and eastern parts of the state. The Pacific Ocean provides abundant moisture, causing frequent precipitation west of the Cascade Mountains, with some locations experiencing orographic enhancement (the increase of rainfall with elevation on the upwind side of mountain ranges). The region east of the Cascades receives less precipitation due to the reduced availability of ocean moisture. Temperatures in the central and eastern portions of the state are not as strongly moderated by the ocean and exhibit a greater annual range than those in the western portion.

Figure 1

Figure 1: Observed and projected changes (compared to the 1901–1960 average) in near-surface air temperature for Washington. Observed data are for 1900–2020. Projected changes for 2006–2100 are from global climate models for two possible futures: one in which greenhouse gas emissions continue to increase (higher emissions) and another in which greenhouse gas emissions increase at a slower rate (lower emissions). Temperatures in Washington (orange line) have risen almost 2°F since the beginning of the 20th century. Shading indicates the range of annual temperatures from the set of models. Observed temperatures are generally within the envelope of model simulations of the historical period (gray shading). Historically unprecedented warming is projected to continue through this century. Less warming is expected under a lower emissions future (the coldest end-of-century projections being about 1°F warmer than the historical average; green shading) and more warming under a higher emissions future (the hottest end-of-century projections being about 10°F warmer than the hottest year in the historical record; red shading). Sources: CISESS and NOAA NCEI.

Since the beginning of the 20th century, temperatures in Washington have risen almost 2°F (Figure 1), and since 1986, all but 5 years have been above the long-term (1895–2020) average. The hottest year on record was 2015, with a statewide average temperature of 50.0°F, which was 3.7°F above the long-term average. The overall warming trend is evident in an increased number of warm nights. Since 1990, the numbers of very cold nights in Eastern Washington and freezing days in Western Washington have both been below average (Figure 2a). However, the numbers of very warm nights in Eastern Washington and warm nights in Western Washington have both been above average since 1990 (Figure 3). The numbers of very hot days in Eastern Washington and hot days in Western Washington have been quite variable but were both generally above average during the 2015–2020 period, after below average numbers during the 2010–2014 period (Figure 2b).

Figure 2

a)

Graph of the observed annual number of very cold nights for eastern Washington (top) and freezing days for western Washington (bottom) from 1900 to 2020 as described in the caption. Y-axis values range from 0 to 20 for both panels. Annual values show year-to-year variability and range from about 0 to 19 very cold nights for eastern Washington and from 0.2 to 18 freezing days for western Washington. Multiyear values for eastern Washington very cold nights show variability. Prior to 1980, they are mostly above the long-term average of 3.7 nights, with the notable exceptions of the 1900 to 1904, 1940 to 1944, 1960 to 1964, and 1965 to 1969 periods. Since 1985, multiyear values are all below average. The 2000 to 2004 period has the lowest multiyear value for very cold nights and the 1920 to 1924 period has the highest. Multiyear values for freezing days in western Washington show a similar pattern of variability, with most periods before 1995 being near or above the long-term average of 3 days, with notable exceptions in 1900 to 1904 and 1940 to 1944. Recent multiyear periods, starting with 1995 to 1999, have all been below average. The highest multiyear values for freezing days occurred in 1920 to 1924 and 1930 to 1934 while the 2000 to 2004 period had the lowest value.

b)

Graph of the observed annual number of very hot days for eastern Washington (top) and hot days for western Washington (bottom) from 1900 to 2020 as described in the caption. Y-axis values range from 0 to 30 very hot days and 0 to 12 hot days. Annual values show year-to-year variability and range from about 3 to 28 very hot days and from 0.8 to about 12 hot days. Between 1900 and 1940, multiyear values for very hot days in eastern Washington are mostly above the long-term average of 14 days, with the exception of the 1900 to 1914 interval. From 1940 to 1989, multiyear values are mostly below average, with the notable exception of the 1970 to 1974 period. Since 1990, multiyear values are mostly above average, with the exception of the 2010 to 2014 period. The 1945 to 1949 period has the lowest multiyear value and the 1970 to 1974 period has the highest. Multiyear averages for hot days in western Washington show variability, with many periods being below the long-term average of 5 days except for the 1905 to 1914 interval, the 1925 to 1944 interval, and the 1955 to 1959, 1985 to 1989, 2005 to 2009, and 2015 to 2020 periods.

c)

d)

Graph of the observed number of 1-inch extreme precipitation events for eastern Washington (top) and 2-inch extreme precipitation events for western Washington (bottom) from 1900 to 2020 as described in the caption. Y-axis values range from 1.5 to 4.5 days for 1-inch events and from 0 to 4 days for 2-inch events. Annual values show year-to-year variability and range from 1.8 to about 4 days for 1-inch events and 0.3 to 3.7 days for 2-inch events. Prior to 1959, multiyear values for 1-inch events in eastern Washington are mostly above the long-term average of 2.5 days, with the exceptions of the 1910 to 1914, 1935 to 1939, and 1940 to 1944 periods. Since 1960, multiyear values are mostly below average, with the exceptions of the 1980 to 1984 and 2015 to 2020 periods. The 1985 to 1989 period has the lowest multiyear period and the 1905 to 1909 period has the highest. Prior to 1980, multiyear values for 2-inch events in western Washington are mostly below the long-term average of 1.5 days, with the exceptions of the 1900 to 1904, 1930 to 1934, and 1935 to 1939 periods. Since 1980, multiyear values are above average, with the exception of the 2010 to 2014 period. The 1940 to 1944 period has the lowest multiyear value and the 1995 to 1999 period has the highest.

Figure 2: Observed (a) annual numbers of very cold nights (minimum temperature of 0°F or lower) for Eastern Washington (top) and freezing days (maximum temperature of 32°F or lower) for Western Washington (bottom), (b) annual numbers of very hot days (maximum temperature of 95°F or higher) for Eastern Washington (top) and hot days (maximum temperature of 90°F or higher) for Western Washington (bottom), (c) total statewide annual precipitation, and (d) annual numbers of 1-inch extreme precipitation events (days with precipitation of 1 inch or more) for Eastern Washington (top) and 2-inch extreme precipitation events (days with precipitation of 2 inches or more) for Western Washington (bottom) from (a, b, d) 1900 to 2020 and (c) 1895 to 2020. Dots show annual values. Bars show averages over 5-year periods (last bar is a 6-year average). The horizontal black lines show the long-term (entire period) averages: (a) 3.7 days (top), 3.0 days (bottom); (b) 14 days (top), 5.0 days (bottom); (c) 42.3 inches; (d) 2.5 days (top), 1.5 days (bottom). (Note that for Figures 2a, 2b, and 2d, the average for individual reporting stations varies greatly because of the state’s large elevation range.) Since 1990, Eastern Washington and Western Washington have experienced below average numbers of very cold nights and freezing days, respectively, which is indicative of warming in the region. The numbers of very hot days in Eastern Washington and hot days in Western Washington have both been variable since 1990. Both annual precipitation and the number of extreme precipitation events have varied widely since the beginning of the 20th century. A typical station in Eastern Washington experiences between two and three 1-inch extreme precipitation events per year. A typical station in Western Washington experiences between one and two 2-inch events per year. Sources: CISESS and NOAA NCEI. Data: (a, b) GHCN-Daily from 17 long-term stations; (c) nClimDiv; (d) GHCN-Daily from 23 long-term stations.

Graph of the observed annual number of very warm nights for eastern Washington (top) and warm nights for western Washington (bottom) from 1900 to 2020 as described in the caption. Y-axis values range from 0 to 12 very warm nights and 0 to 14 warm nights. Annual values show variability and range from 0.9 to about 11 very warm nights and from 0.1 to about 12 warm nights. Prior to 1990, multiyear values for eastern Washington are mostly near or below the long-term average of 4.1 nights. Since 1990, multiyear values are all above average. The 1945 to 1949 period has the lowest multiyear value and the 2005 to 2009 period has the highest. Prior to 1990, multiyear values for western Washington are mostly below the long-term average of 3.2 nights, with the exceptions of the 1925 to 1929, 1940 to 1944, and 1955 to1959 periods. Since 1990, multiyear values are all above average. The 1975 to 1979 period has the lowest multiyear value and the 1995 to 1999 period has the highest.

Figure 3: Observed annual numbers of very warm nights (minimum temperature of 65°F or higher) for Eastern Washington and warm nights (minimum temperature of 60°F or higher) for Western Washington from 1900 to 2020. Dots show annual values. Bars show averages over 5-year periods (last bar is a 6-year average). The horizontal black lines show the long-term (entire period) averages of 4.0 nights (top) and 2.5 nights (bottom; note that the average for individual reporting stations varies greatly because of the state’s large elevation range). The numbers of very warm nights in Eastern Washington and warm nights in Western Washington have both been above average since 1900. Sources: CISESS and NOAA NCEI. Data: GHCN-Daily from 17 long-term stations.

Annual precipitation exhibits wide regional variations across the state. Portions of the Olympic Peninsula receive upwards of 150 inches of precipitation annually, while areas along the Columbia River in eastern interior Washington average less than 10 inches. Statewide total annual precipitation has ranged from a low of 26.0 inches in 1929 to a high of 55.0 inches in 1996. The driest multiyear periods were in the late 1920s, early 1940s, and late 1980s, and the wettest were in the early 1970s, early 1980s, and late 1990s (Figure 2c). The driest consecutive 5-year interval was 1926–1930, with an annual average of 34.6 inches, and the wettest was 1995–1999, with an annual average of 51.0 inches. Washington has not experienced any long-term trend in the number of extreme precipitation events (Figure 2d).

Most of Washington’s precipitation falls during the winter months, and the Cascades can receive upwards of 400 inches of snowfall annually. Snowpack in the mountains provides an important source of water during the drier summer months (Figure 4). Precipitation falling as rain rather than snow can have negative impacts on critical industries, such as timber and agriculture, which are also vulnerable to extreme temperatures. Wildfires during the drier summer months are a particular concern. The 2015 wildfire season was the most destructive in Washington’s history, with more than 1 million acres burned (more than 6 times the average).

Figure 4: Variations in April 1 snow water equivalent (SWE) at the Fish Lake, Washington, snow course site from 1943 to 2019. SWE, the amount of water contained within the snowpack, varies widely from year to year, but there is a general downward trend. The extremely low snowpack levels in 2005 (third lowest) were due to below average winter precipitation and above average winter temperatures. In 2015 (record lowest), warmer than normal winter temperatures were the main driver of the drought, causing more precipitation to fall as rain rather than snow. Source: NRCS NWCC.

Under a higher emissions pathway, historically unprecedented warming is projected to continue through the end of this century (Figure 1). Even under a lower emissions pathway, temperatures are projected to most likely exceed historical record levels by the middle of this century. However, a large range of temperature increases is projected under both pathways, and under the lower pathway, a few projections are only slightly warmer than historical records (Figure 1). Overall, warming will lead to increases in heat wave intensities but decreases in cold wave intensities. Unlike other locations in the United States, Seattle and other urban areas are rarely exposed to very high temperatures. Future heat waves, particularly an increase in the frequency of warm nights, could stress these communities, which are not well adapted to such events.

Temperature increases will affect basins with significant snowmelt contributions to their streamflow. Projected rising temperatures will raise the elevation of the snow line—the average lowest elevation at which snow falls. This will increase the likelihood that precipitation will fall as rain instead of snow, reducing water storage in the snowpack, particularly at those lower mountain elevations that are now on the margins of reliable snowpack accumulation. Rainfall is expected to be the dominant form of precipitation across the majority of the state by the end of this century. Higher spring temperatures will also result in earlier melting of the snowpack, with average snowpack projected to decline by up to 70% by the end of this century. This will further decrease water availability during the already dry summer months, and due to earlier spring peak flows, it will increase the risk of spring flooding. Projected increases in heavy rainfall events by midcentury could further increase flood risk. Reductions in summer flow (projected to occur in 80% of the state’s watersheds) will have important ecological implications and are a particular concern for hydropower and irrigation water supplies.

Increasing temperatures raise concerns for sea level rise in coastal areas. Since 1900, global average sea level has risen by about 7–8 inches. It is projected to rise another 1–8 feet, with a likely range of 1–4 feet, by 2100 as a result of both past and future emissions from human activities (Figure 6). Sea level rise has caused an increase in tidal floods associated with nuisance-level impacts. Nuisance floods are events in which water levels exceed the local threshold (set by NOAA’s National Weather Service) for minor impacts. These events can damage infrastructure, cause road closures, and overwhelm storm drains. As sea level has risen along the Washington coastline, the number of tidal flood days has also increased at Seattle, with the greatest number (11) occurring in 1997 during a strong El Niño event (Figure 7). Some areas of the coast are rising, which has mitigated the impacts of recent sea level rise and will reduce somewhat the local projected sea level rise.

Although projections of overall annual precipitation are uncertain, summer precipitation is projected to decrease (Figure 5). Drier conditions during the summer could increase reliance on diminishing snowmelt for irrigation. Additionally, the combination of drier summers, higher temperatures, and earlier melting of the snowpack would tend to increase the frequency and extent of wildfires.

Map of the contiguous United States showing the projected changes in total summer precipitation by the middle of this century as described in the caption. Values range from less than minus 20 to greater than positive 15 percent. Summer precipitation is projected to increase along the east coast and decrease across most of the rest of the country, particularly in Oregon and California. Statistically significant increases are projected for southeastern North Carolina and northern Maine. The projected change in summer precipitation is uncertain for some areas in the north-central United States, New Mexico, and northern Florida. Statistically significant decreases are projected for portions of the central United States. Almost all of Washington is projected to see a decrease of 5 to 10 percent, with two small areas in the southwest and southeast portions of the state projected to see decreases of 10 to 15 percent.

Figure 5: Projected changes in total summer (June–August) precipitation (%) for the middle of the 21st century compared to the late 20th century under a higher emissions pathway. Whited-out areas indicate that the climate models are uncertain about the direction of change. Hatching represents areas where the majority of climate models indicate a statistically significant change. Washington is projected to see a decrease in summer precipitation. Source: CISESS. Data: CMIP5.

Figure 6: Global mean sea level (GMSL) change from 1800 to 2100. Projections include the six U.S. Interagency Sea Level Rise Task Force GMSL scenarios (Low, navy blue; Intermediate-Low, royal blue; Intermediate, cyan; Intermediate-High, green; High, orange; and Extreme, red curves) relative to historical geological, tide gauge, and satellite altimeter GMSL reconstructions from 1800–2015 (black and magenta lines) and the very likely ranges in 2100 under both lower and higher emissions futures (teal and dark red boxes). Global sea level rise projections range from 1 to 8 feet by 2100, with a likely range of 1 to 4 feet. Source: adapted from Sweet et al. 2017.

Graph of the observed and projected annual number of tidal flood days at Seattle, Washington, from 1920 to 2100 (top panel) as described in the caption. The bottom panel is a magnified view of the observed data. In the top panel, y-axis labels range from 0 to 400 days, with a dashed line indicating the maximum possible number of tidal flood days per year (365). In the bottom panel, y-axis values range from 0 to 15 days, and observed values range from 0 to 11 days. Since the first recorded event in 1920 until 2002, tidal flooding was sporadic, often with gaps of 1 to 3 years between events and annual values mostly below 4 days. Since 2002, tidal flood days have occurred almost every year, with the record high of 11 in 1997. Seattle is projected to experience about 11 to 27 tidal flood days by 2050 under the Intermediate-Low and Intermediate scenarios, respectively, and about 66 to 334 days by 2100.

Figure 7: Number of tidal flood days per year at Seattle, Washington, for the observed record (1920–2020 orange bars) and projections for two NOAA (2017) sea level rise scenarios (2021–2100): Intermediate (dark blue bars) and Intermediate-Low (light blue bars). The NOAA (2017) scenarios are based on local projections of the GMSL scenarios shown in Figure 5. Sea level rise has caused a gradual increase in tidal floods associated with nuisance-level impacts. The greatest number of tidal flood days (all days exceeding the nuisance-level threshold) occurred in 1997 at Seattle. Projected increases are large even under the Intermediate-Low scenario. Under the Intermediate scenario, tidal flooding is projected to occur nearly every day of the year by the end of the century. Additional information on tidal flooding observations and scenarios is available online at https://statesummaries.ncics.org/technicaldetails. Sources: CISESS and NOAA NOS.

Details on observations and projections are available on the Technical Details and Additional Information page.

Lead Authors
Contributing Authors
Recommended Citation: Frankson, R., K.E. Kunkel, S.M. Champion, D.R. Easterling, L.E. Stevens, K. Bumbaco, N. Bond, J. Casola, and W. Sweet, 2022: Washington State Climate Summary 2022. NOAA Technical Report NESDIS 150-WA. NOAA/NESDIS, Silver Spring, MD, 5 pp.

RESOURCES

Bumbaco, K.A., K.D. Dello, and N.A. Bond, 2013: History of Pacific Northwest heat waves: Synoptic pattern and trends. Journal of Applied Meteorology and Climatology, 52 (7), 1618–1631. http://dx.doi.org/10.1175/jamc-d-12-094.1
Hayhoe, K., D.J. Wuebbles, D.R. Easterling, D.W. Fahey, S. Doherty, J. Kossin, W. Sweet, R. Vose, and M. Wehner, 2018: Our changing climate. In: Impacts, Risks, and Adaptation in the United States: Fourth National Climate Assessment, Volume II. Reidmiller, D.R., C.W. Avery, D.R. Easterling, K.E. Kunkel, K.L.M. Lewis, T.K. Maycock, and B.C. Stewart, Eds. U.S. Global Change Research Program, Washington, DC, 72–144. https://nca2018.globalchange.gov/chapter/2/
Kunkel, K.E., L.E. Stevens, S.E. Stevens, L. Sun, E. Janssen, D. Wuebbles, K.T. Redmond, and J.G. Dobson, 2013: Regional Climate Trends and Scenarios for the U.S. National Climate Assessment Part 6. Climate of the Northwest U.S. NOAA Technical Report NESDIS 142-6. National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, Silver Spring, MD, 83 pp. https://nesdis-prod.s3.amazonaws.com/migrated/NOAA_NESDIS_Tech_Report_142-6-Climate_of_the_Northwest_U.S.pdf
Miller, I.M., H. Morgan, G. Mauger, T. Newton, R. Weldon, D. Schmidt, M. Welch, and E. Grossman, 2018: Projected Sea Level Rise for Washington State—A 2018 Assessment. A collaboration of Washington Sea Grant, University of Washington Climate Impacts Group, University of Oregon, University of Washington, and U.S. Geological Survey. Prepared for the Washington Coastal Resilience Project. Updated July 2019. Climate Impacts Group, University of Washington, Seattle, WA. https://cig.uw.edu/resources/special-reports/sea-level-rise-in-washington-state-a-2018-assessment/
NAS, 2012: California sea level projected to rise at higher rate than global average; slower rate for Oregon, Washington, but major earthquake could cause sudden rise. News from the National Academies. National Academy of Sciences, Washington, DC. https://web.archive.org/web/20120627090639/http://www8.nationalacademies.org/onpinews/newsitem.aspx?RecordID=13389
NOAA NCDC, n.d.: Climate of Washington. National Oceanic and Atmospheric Administration, National Climatic Data Center, Asheville, NC, 13 pp. https://www.ncei.noaa.gov/data/climate-normals-deprecated/access/clim60/states/Clim_WA_01.pdf
NOAA NCEI, 2014: State of the Climate: National Climate Report for July 2014. National Oceanic and Atmospheric Administration, National Centers for Environmental Information, Asheville, NC. https://www.ncdc.noaa.gov/sotc/national/201407
NOAA NCEI, n.d.: Climate at a Glance: Statewide Time Series, Washington. National Oceanic and Atmospheric Administration, Asheville, NC, accessed July 2, 2021. https://www.ncdc.noaa.gov/cag/statewide/time-series/45/
NRCS NWCC, n.d.: Snowpack: Snow Water Equivalent (SWE) and Snow Depth [Fish Lake, WA]. Natural Resources Conservation Service, National Water and Climate Center, Portland, OR. https://www.nrcs.usda.gov/wps/portal/wcc/home/snowClimateMonitoring/snowpack/
Snover, A.K., G.S. Mauger, L.C. Whitely Binder, M. Krosby, and I. Tohver, 2013: Climate Change Impacts and Adaptation in Washington State: Technical Summaries for Decision Makers. State of Knowledge Report prepared for the Washington State Department of Ecology. Climate Impacts Group, University of Washington, Seattle, WA, 130 pp. https://cig.uw.edu/wp-content/uploads/sites/2/2020/12/snoveretalsok816.pdf
Sweet, W., G. Dusek, J. Obeysekera, and J. Marra, 2018: Patterns and Projections of High Tide Flooding Along the U.S. Coastline Using a Common Impact Threshold. NOAA Technical Report NOS CO-OPS 086. National Oceanic and Atmospheric Administration, National Ocean Service, Center for Operational Oceanographic Products and Services, Silver Spring, MD, 56 pp. https://tidesandcurrents.noaa.gov/publications/techrpt86_PaP_of_HTFlooding.pdf
Sweet, W., S. Simon, G. Dusek, D. Marcy, W. Brooks, M. Pendleton, and J. Marra, 2021: 2021 State of High Tide Flooding and Annual Outlook. NOAA High Tide Flooding Report. National Oceanic and Atmospheric Administration, National Ocean Service, Center for Operational Oceanographic Products and Services, Silver Spring, MD, 28 pp. https://tidesandcurrents.noaa.gov/publications/2021_State_of_High_Tide_Flooding_and_Annual_Outlook_Final.pdf
Sweet, W.V., R.E. Kopp, C.P. Weaver, J. Obeysekera, R.M. Horton, E.R. Thieler, and C. Zervas, 2017: Global and Regional Sea Level Rise Scenarios for the United States. NOAA Technical Report NOS CO-OPS 083. National Oceanic and Atmospheric Administration, National Ocean Service, Center for Operational Oceanographic Products and Services, Silver Spring, MD, 75 pp. https://tidesandcurrents.noaa.gov/publications/techrpt83_Global_and_Regional_SLR_Scenarios_for_the_US_final.pdf
Vose, R.S., D.R. Easterling, K.E. Kunkel, A.N. LeGrande, and M.F. Wehner, 2017: Temperature changes in the United States. In: Climate Science Special Report: Fourth National Climate Assessment, Volume I. Wuebbles, D.J., D.W. Fahey, K.A. Hibbard, D.J. Dokken, B.C. Stewart, and T.K. Maycock, Eds. U.S. Global Change Research Program, Washington, DC, 185–206. http://doi.org/10.7930/J0N29V45

NOAA National Centers
for Environmental Information

State Climate Summaries 2022

WASHINGTON

Key Message 1

Key Message 2

Key Message 3

WASHINGTON

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