The Columbia Basin Climate Change Scenarios Project (CBCCSP) was conceived as a comprehensive hydrologic database to support climate change planning, impacts assessment, and adaptation in the Pacific Northwest (PNW) by a diverse user community with varying technical capacity over a wide range of spatial scales. July temperatures hover in the 90s, with several afternoons during the summer pushing the thermometer reading as high as 100 to 105 degrees. How do I view content? (2005). Detailed forecast for Lower Columbia Basin of Washington Rest Of Today Partly sunny. These include the following: Columbia River Basin Impact Assessment: Reclamation conducted the Columbia River Basin Impact Assessment to evaluate the potential effects of future climate change on river flows at 158 locations across the basin. 2013b. 5 Examples of summary plots for monthly snow water equivalent (SWE) (mm) (averaged over the upstream basin area) and raw streamflow not adjusted for bias (cubic metres per second) for the Skagit River at Mount Vernon. Ten GCM projections for the A1B scenario and nine projections for the B1 scenario (Table 1) were selected based on a ranking of the GCMs reflecting the combined ability of each GCM to reproduce key features of PNW climate variability, including the seasonal cycle of precipitation, observed trends in temperature in the late twentieth century, bias in reproducing historical temperature and precipitation, and ability to capture key features of observed climate variability (spatial patterns of temperature, pressure, and precipitation) over the North Pacific (Mote & Salath, Citation2010). The climate of the high mountain regionsthe pramos, ranging from about 10,000 to 15,000 feet (3,000 to 4,600 metres)is characterized by average temperatures below 50 F (10 C), fog, overcast skies, frequent winds, and light rain or drizzle. Casola, J. H., Kay, J. E., Snover, A. K., Norheim, R. A., Binder, L. C. W., & the Climate Impacts Group. Highs in the lower to mid 60s. Source: Bonneville Power Administration. These lands are those without any sort of status that provides government protection, such as an indigenous territory, or that have not . Blue traces show monthly averages for historical conditions; the pink bands show the range of projected change associated with each scenario and future time period; the red lines show the average of the future ensemble. Lee. In addition to the time series gridded data, the long-term monthly mean data for each hydrologic variable, for each scenario, is provided in GridASCII format, compatible with ArcGIS. Economic value of long-lead streamflow forecasts for Columbia River hydropower, Effects of projected climate change on energy supply and demand in the Pacific Northwest and Washington State, Columbia River streamflow forecasting based on ENSO and PDO climate signals, Effects of climate change on hydrology and water resources in the Columbia River basin, Long-range climate forecasting and its use for water management in the Pacific Northwest Region of North America, Production of temporally consistent gridded precipitation and temperature fields for the continental U.S, Effects of 20th century warming and climate variability on flood risk in the western U.S, Effects of temperature and precipitation variability on snowpack trends in the western U.S, An improved method for estimating surface humidity from daily minimum temperature, Optimized flood control in the Columbia River basin for a global warming scenario, Methodology for developing flood rule curves conditioned on El Nio-Southern Oscillation classification, Daily time step refinement of optimized flood control rule curves for a global warming scenario, Improving water resources system performance through long-range climate forecasts: The Pacific Northwest experience (Chapter 7), Water resources implications of global warming, a U.S. regional perspective, Simulations of the ENSO hydroclimate signals in the Pacific Northwest Columbia River basin, A simple hydrologically based model of land surface water and energy fluxes for general circulation models. Detailed forecast for Upper Columbia Basin Tonight Mostly clear. Hydrologic sensitivity of global rivers to climate change. The site at Corra Linn Dam on the Kootenay River is representative of changing hydrographs in many locations in the northern tip of the CRB in British Columbia. Climate Resilience Program - Columbia Basin Trust Elsner MM, et al. The same basic effects are seen in the SWE2PR maps, where snowmelt remains dominant in the northern tip of the CRB even at the end of the twenty-first century, whereas in the US portions of the domain there are widespread transformations of mixed-rain-and-snow river basins to rain-dominant basins and snowmelt-dominant basins to mixed-rain-and-snow basins. Did you know that with a free Taylor & Francis Online account you can gain access to the following benefits? Climate Change Impacts on Columbia River Basin Fish and Wildlife The macroscale hydrologic model used in the CBCCSP is the VIC model (Cherkauer & Lettenmaier, Citation2003; Liang, Lettenmaier, Wood, & Burges, Citation1994) implemented at 1/16 degree resolution. The most sensitive basins are mixed-rain-and-snow basins. Hamlet, and S.-Y. Snover, A. K., Hamlet, A. F., Lee, S.-Y., Mantua, N. J., Salath, E. P. Jr, Steed, R., & Tohver, I. 2013a. 120 0 obj <>/Filter/FlateDecode/ID[<6FB239FABFBE0241AD2ED78CAB939AAB><0AF5FFF7A9777A438917926E6F546C9A>]/Index[95 41]/Info 94 0 R/Length 116/Prev 312890/Root 96 0 R/Size 136/Type/XRef/W[1 3 1]>>stream NWPCC (Northwest Power and Conservation Council). Even with substantial cuts to greenhouse gas emissions, scientists expect our climate to continue changing over the coming decades. The study employs a state-of-the-art, end-to-end data processing sequence that moves from raw GCM output to a set of final hydrological products that can be accessed by the user community from a web-accessible database. 1990 level modified streamflow 19281989. Prior climate change datasets for the CRB produced by CIG (using CMIP2/TAR projections) only included about 20 river sites (e.g., NWPCC, Citation2005; Snover et al., Citation2003) and provided very limited support for planning efforts at smaller spatial scales. Changes in snowpack are a key driver of hydrologic impacts in the PNW (Elsner et al., Citation2010; Hamlet & Lettenmaier, Citation1999b). Detailed information about the study can be found under Documentation, while model results can be found under Data. Get the forecast for today, tonight & tomorrow's weather for Guarant do Norte, Mato Grosso, Brazil. About 15 sites in western Washington, outside the CRB, were also included in support of the 2009 WACCIA. Although a number of pilot climate change studies have been carried out in the CRB in collaboration with various water management agencies in the past (e.g., NWPCC, Citation2005), the RMJOC study was something of a landmark in that it was the first time that the BPA, USBR, and USACE used climate change information in coordinated interagency planning exercises in the CRB. Saturday Night And Sunday: Cloudy with a 50 percent chance of rain. Highs in the lower to mid 40s. Tague, Grant, Farrell, Choate and Jefferson (Citation2008) showed analogous differences between watersheds in the PNW based on the relative contribution of groundwater to base flows. The MOCOM-UA tool uses an objective function (defined by the user) and a shuffle complex evolution procedure to optimize model calibration parameters to create a set of Pareto (equally) optimal calibration parameters. Lows in the lower to mid 30s. How essential is hydrologic model calibration to seasonal streamflow forecasting? To learn about our use of cookies and how you can manage your cookie settings, please see our Cookie Policy. Current weather in Queens Cup Basin and forecast for today, tomorrow, and next 14 days Thus, depending on their needs and level of technical sophistication, stakeholders can make the best use of the study products by extracting information at different points in the data processing sequence, all of which are available on the study web site. RSUM[Traduit par la rdaction] Le projet de scnarios de changement climatique du bassin du Columbia (CBCCSP) a t conu comme une base de donnes hydrologiques complte pour appuyer les activits de planification, dvaluation des rpercussions et d'adaptation dans la rgion pacifique nordouest menes par une communaut d'utilisateurs diversifie disposant de capacits techniques varies dans une large gamme dchelles spatiales. A family of greenhouse gas emissions scenarios used in the IPCC effort (Nakienovi et al. Using these resources, other modelling groups can carry out their own investigations of hydrologic impacts using either their own hydrologic model (just using the driving data) or the VIC implementation from the CBCCSP. Columbia Basin Care is the region's only independent nonprofit skilled nursing facility for long-term care and short-term rehabilitation. Table 1 summarizes the 77 future meteorological forcing datasets that were prepared for the study. Blue dots represent the historical values; the red dots show the range of values from the HD ensemble (10 or 9 values); black dashes show the mean of the HD ensemble, and the orange dots show the single value calculated for the CD projections. Based on, Learn more about the impacts of climate change, Learn how the climate is changing in your area, Learn how our region is responding, and how you can be part of the solution, BC Ministry of Forests, Lands, Natural Resource Operations and Rural Development. Special thanks to Kurt Unger and Ken Slattery, who were the primary architects of the CBCCSP at WDOE. Temperature and precipitation vary greatly with elevation, but in the central basin January average daily temperatures are between about 25 and 30 F (4 and 1 C), and July averages are mostly between 70 and 75 F (21 and 24 C). The USFS and USFWS studies have supported a number of high-visibility ecosystem studies, including assessment of the impacts of changing snowpack on wolverine populations (McKelvey et al., Citation2011) and subsequent proposed ESA listing of wolverine populations, and comprehensive assessment of climate change impacts to trout species over the west (Wenger et al., Citation2011). O weather.com oferece para voc a previso do tempo mais precisa para Guarant do Norte, Mato Grosso com mdias/recordes e temperaturas mximas/mnimas, precipitaes e muito mais. Associated shifts in streamflow timing from spring and summer to winter are also evident in basins with significant snow accumulation in winter (for the current climate). The authors would like to acknowledge the contributions of two anonymous reviewers and the lead and associate editors for Atmosphere-Ocean, whose constructive suggestions substantially improved the paper during the review process. The Climate of the Columbia Plateau in Washington State (Citation2010) over the entire PNW (Tohver et al. About 50 of the 80 sites evaluated show monthly NSE scores greater than or equal to approximately 0.7 (good to excellent fit). Les rsultats de ltude montrent de profonds changements dans l'accumulation de neige au printemps et des dplacements radicaux de neige ou pluie et neige mles vers principalement pluie dans presque tout le domaine. The Columbia Basin-Boundary region is already experiencing a climate that's different from 50 years ago. For climate change studies in the western United States where snow is an important element of the hydrologic cycle, the model's use of a sophisticated energy-balance snow model, which incorporates important effects on snow accumulation and melt associated with vegetation canopy (Andreadis, Storck, & Lettenmaier, Citation2009) has been a notable advantage. In 2021, these livestock operations alone accounted for 75% of deforestation on public lands, according to a study by the Amazon Environmental Research Institute (IPAM).. Sites without modified or natural flow estimates are shown in yellow. Monthly hydrographs in different portions of the domain primarily reflect changes in snow accumulation and melt processes and seasonal changes in precipitation (generally wetter falls, winters, and springs and drier summers). Figure 1 shows a map of the approximately 300 streamflow locations that were ultimately compiled from these lists for inclusion in the study (a spreadsheet listing these sites is available on the CBCCSP website (CIG, Citation2013a)). The state of Oregon, for example, is classified as about 75% mixed-rain-and-snow for the twentieth century climate. Determining surface water availability in Oregon. Following the WACCIA in 2009, the WA Legislature, via the Act relating to State Agency Climate Leadership (2009), charged WDOE and other state agencies with preparing a first climate change adaptation plan for WA. Thus, by selecting 10 GCM scenarios with good historical performance that also spanned the range of impacts, we effectively reduced the computational and storage requirements of the CBCCSP by approximately a factor of two. Gridded meteorological datasets (daily total precipitation and maximum and minimum daily temperature) at 1/16 degree latitude-longitude resolution (approximately 7km by 5km) were constructed for the study from observed station records for the period 1915 to 2006. Simulation of spatial variability in snow and frozen soil, A multi-model ensemble approach to assessment of climate change impacts on the hydrology and water resources of the Colorado River basin, CIG (Climate Impacts Group). This is likely because soil moisture is higher in summer west of the Cascade Range and evapotranspiration is mostly energy limited, whereas east of the mountains the late summer soil moisture is already very low in the current climate and increasing evapotranspiration does not result in much additional soil moisture stress. Gusts up to 20 mph in the morning. The Columbia Basin-Boundary region is already experiencing a climate thats different from 50 years ago. Lvapotranspiration potentielle augmente dans la majeure partie de la rgion du Pacifique et du NordOuest en t cause des tempratures plus leves; cependant, lvaporation relle est rduite dans presque tous les secteurs du domaine parce que lvapotranspiration est principalement limite par l'eau en t et les prcipitations estivales diminuent dans les simulations. Bias corrected inflows were produced to support the GENESYS and HYDSIM reservoir operations models, which are used by the NWPCC and BPA, respectively, for main-stem studies in the CRB (e.g., NWPCC, Citation2005). Retrieved from, CIG (Climate Impacts Group). Weather for Queens Cup Basin, British Columbia, Canada Lows in the lower 50s. Zone Area Forecast for Lower Columbia Basin of Washington Cited by lists all citing articles based on Crossref citations.Articles with the Crossref icon will open in a new tab. Statistics for hydrologic extreme events (as discussed above) are presented in a different format, shown in Fig. The VIC model (version 4.0.7) was implemented at 1/16 degree resolution, with three active soil layers and up to five elevation bands with an approximate spacing of 500m. The model was run in water balance mode with a snow model time step of 1h and a water balance time step of 24h. The model was coupled to a simple daily-time-step routing model (Lohmann, Raschke, Nijssen, & Lettenmaier, Citation1998), which was used to produce daily flow estimates at each of the approximately 300 streamflow locations included in the study. Among its most useful features is the predominantly physical basis of the model, which largely avoids concerns about parameter stationarity in a changing climate. Monday: A chance of snow before 4 p.m., then a slight chance of rain and snow. Hydrology and water resources research at CIG was particularly focused on the use of experimental climate and hydrologic forecasts for the CRB (Hamlet & Lettenmaier, Citation1999a, Citation2000; Lettenmaier & Hamlet, Citation2003; Leung, Hamlet, Lettenmaier, & Kumar, Citation1999) in the context of decision support for various water management applications (Hamlet, Huppert, & Lettenmaier, Citation2002; Lee, Hamlet, Fitzgerald, & Burges, Citation2011; Voisin et al., Citation2006). The Climate Resilience Program helps communities in the Basin become more climate resilient by supporting large-scale, multi-year, shovel-ready climate mitigation, adaptation, and resilience projects that address sources of climate change or manage the risks of climate change impacts. Many river locations that were submitted for consideration were at gauging locations supported by the USGS and ECAN, or at locations associated with important water resources monitoring needs (e.g., checkpoints for flood control, water supply, or environmental flows) or infrastructure (e.g., dams and diversion points). Southwest wind 5 to 15 mph with gusts to around 25 mph. 135 0 obj <>stream Mitigating the effects of climate change on the water resources of the Columbia River basin, Downscaling simulations of future global climate with application to hydrologic modeling, Review of scenario selection and downscaling methods for the assessment of climate change impacts on hydrology in the United States Pacific Northwest. (Citation2010). Results from the study show profound changes in spring snowpack and fundamental shifts from snow and mixed-rain-and-snow to rain-dominant behaviour across most of the domain. The VIC implementations make use of preprocessed soil and vegetation databases for the basin of interest. Fig. 8 Monthly mean hydrographs not adjusted for bias (water year: OctoberSeptember) for four representative river sites in the PNW: Kootenay River at Corra Linn Dam (upper left), Columbia River at The Dalles, Oregon (upper right), Yakima River at Parker (lower left), and the Chehalis River at Grand Mound (lower right). In other words, although at these sites the model results do not match the observations in the absolute sense (large bias), the relative changes follow the observed variations quite well (high R 2). Ingalls Weather - Weather reports on whatever I decide to report on. The authors would like to acknowledge the contributions of other members of the CBCCSP research team at the UW including Lara Whitely Binder, Pablo Carrasco, Jeffrey Deems, Carrie Lee, Dennis P. Lettenmaier, Tyler Kamstra, Jeremy Littell, Nathan Mantua, Edward Miles, Kristian Mickelson, Philip W. Mote, Erin Rogers, Eric Salath, Amy Snover, and Andrew Wood. In this case only modified flows (2000-level modified flows obtained from the BPA (Crook, Citation1993)) were used to train the bias-correction procedure, even if naturalized flows were also available. The city's average temperature is 57 F (14 C). As mentioned above, 20062007 was something of a turning point for regional stakeholders considering future actions to prepare for climate change. These results point to extensive, landscape-scale transformations in hydrologic behaviour associated with climate change. The DOI via the USFWS has recently established a set of LCCs across the United States (USFWS, Citation2013) and has generated additional funding to support a group of regional CSCs, one of which was recently established in the PNW (PNWCSC), combining the efforts of about 15 PNW research universities, jointly led by the USGS, Oregon State University, the UW, and the University of Idaho. A comprehensive website was to be developed to serve all the data produced by the study, at no cost, to the general public, management professionals agency staff members, scientific researchers, private sector consultants, etc. This daily disaggregation technique sometimes introduces an undesirable discontinuity in the bias-corrected daily values at the beginning and end of months. Why is a 1C increase such a big deal? endstream endobj startxref Daily and monthly streamflow for each streamflow site are provided in two formats: a) raw VIC simulations, and b) bias-adjusted simulations. Evidence includes increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global mean sea level. Saturday: Mostly cloudy with a 20 percent chance of rain. This web site provides streamflow information for the Columbia River and coastal drainages in Washington and Oregon State for the 21st century based on a large number of climate scenarios and model experiments. Figure 8 shows hydrographs from selected basins with different hydrologic classifications (snowmelt-dominant, mixed-rain-and-snow, and rain-dominant) in the United States and Canada. unpublished manuscript). Lows in the upper 30s to lower 40s. Right panel: Historical estimates of summer AET (upper right) compared with percentage changes for the same CD scenarios. 6. Oregon Water Resources Department. The summary figures for water balance variables at each site have the same format, two examples of which are shown in Fig. Hamlet, A. F., Carrasco, P., Deems, J., Elsner, M. M., Kamstra, T., Lee, C., Lee, S-Y, Mauger, G., Salathe, E. P., Tohver, I., & Binder, L. W. (2010a). Peak flows actually increase at many sites in Canada because of increasing fall, winter, and spring precipitation in this part of the domain, although the peak flow also occurs about a month earlier. For example, to support academic or agency researchers with their own hydrologic modelling capability, the study provides projections of meteorological drivers such as temperature, precipitation, solar radiation, and humidity and a calibrated VIC hydrologic model implementation. Contract # DE-AC79-92BP21985. Des accroissements gnraliss simuls de la rhumidification du sol en automne et en hiver dans les secteurs o l'accumulation de neige en hiver est importante (sous le climat actuel) appuient les hypothses de risque accru de glissement de terrain et de transport de sdiments durant l'hiver dans le futur. Tonight Mostly cloudy. (Citation2010). The largest reductions in low flows occur west of the Cascade Range in the simulations. 8). Other climate change studies on the Columbia River and its sub-basins followed (Cohen, Miller, Hamlet, & Avis, Citation2000; Elsner et al., Citation2010; Hamlet, Citation2003, Citation2011; Hamlet, Lee, Mickelson, & Elsner, Citation2010b; Lee, Fitzgerald, Hamlet, & Burges, Citation2011; Lee, Hamlet, Fitzgerald, & Burges, Citation2009; NWPCC, Citation2005; Payne, Wood, Hamlet, Palmer, & Lettenmaier, Citation2004; Snover, Hamlet, & Lettenmaier, Citation2003; Vano et al., Citation2010). Post-processing of the primary VIC model output (see Table 2) was carried out to produce a number of specific products discussed in the following sections. Hydrologic climate change scenarios for the Pacific Northwest Columbia River basin and coastal drainages. To produce the bias-adjusted flows, a bias correction procedure using quantile mapping techniques is applied (Elsner et al., Citation2010; Snover et al., Citation2003; Vano et al., Citation2010). Fig. Obtain permissions instantly via Rightslink by clicking on the button below: If you are unable to obtain permissions via Rightslink, please complete and submit this Permissions form. Source: These products are based solely on the HD projections listed in Table 1. Fig. Basin topographic map and smoothed basin boundary at 1/16 degree resolution. Future work on the project will likely focus on expanding the number of streamflow sites for which products are available (e.g., inclusion of additional sites in coastal Oregon in the site-specific products) and providing a comprehensive suite of products associated with CMIP5 results (Taylor, Stouffer, & Meehl, Citation2012) associated with IPCC AR5. The CBCCSP had a budget of about US$500 thousand (in 2010 dollars) over two years. Fig. After fitting three-parameter generalized extreme value probability distributions to the annual peak flow data, the daily 20-, 50-, and 100-year floods (under natural flow conditions) are estimated for both historical and future periods. Highs in the lower to mid 40s. It is important to acknowledge that opinions differ on the utility or even possibility of improving ensembles of future projections based on the ability to simulate the past climate (e.g., Gleckler, Taylor, & Doutriaux, Citation2008). The scope of work for the project called for hydrologic modellers at CIG to produce the following results: A suite of up-to-date hydrologic projections for the entire CRB (including portions of the basin in Canada) based on the CMIP3/AR4 (Meehl et al., Citation2007) GCM projections. Simulations of floods and extreme low flows increase in intensity for most of the river sites included in the study. Colombia - Climate | Britannica Thus, each site is bias-corrected using either naturalized or modified flow but not both. These areas are so cold in winter (DJF average on the order of -10C temperature) that a change in temperatures of 23C has relatively little effect on seasonal snow accumulation in the 2020s and 2040s. The BCSD runs are transient runs from 1950 to 2098 or 1950 to 2099 (depending on the GCM). Figure 10 shows a map of Q100 ratios (future Q100 to historical Q100) for 297 river locations and a scatterplot of the Q100 ratio as a function of winter temperature regime in each basin. hbbd```b``z"I09 D.^`,L,=`v0fI" IA$C(QDrML@a`ig c An understanding of the basin's transboundary nature has also informed CIG's hydrologic modelling studies, which have consistently provided complete coverage of the Canadian and US portions of the basin. The process was also significantly improved by researchers at PCIC who reconfigured and optimized the code to run more efficiently on a Linux cluster (Schnorbus, Bennett, Werner, & Berland, Citation2011). Since its inception in 1995, CIG has been extensively involved in climate-related research focused on the CRB and its water resources management systems. Daily streamflow data from the CD and HD downscaling methods are first processed to extract the peak daily flow in each water year of the simulations (91 years). In particular, it is clear that Canada will have not only about 50% of the reservoir storage in the CRB (Hamlet, Citation2003) but also an increasingly dominant portion of the natural water storage as snowpack in the future. Highs around 80. Those who wish to do additional post-processing of the existing VIC data can access the archived model output. endstream endobj 96 0 obj <. Naturalized streamflow data were used exclusively in the CBCCSP to calibrate the hydrologic model. Potential evapotranspiration increases over most of the PNW in summer because of rising temperatures; however, actual evapotranspiration is reduced in all but a few areas of the domain because evapotranspiration is mostly water limited in summer, and summer precipitation decreases in the simulations. What Makes The Columbia River Basin Unique and How We Benefit We should note that glaciers and deep groundwater (e.g., contributions to streamflow from large confined aquifers) are not simulated by the VIC model, and impacts in areas profoundly influenced by these hydrologic features may not be well characterized in the simulations (Wenger et al., Citation2010). Preparing for climatic change: The water, salmon, and forests of the Pacific Northwest. The study has constructed a state-of-the-art, end-to-end data processing sequence from raw climate model output to a suite of hydrologic modelling products that are served to the user community from a web-accessible database. This extreme scenario, however, was only run by a few GCMs, which ultimately limits the ability to show consistent ranges of outcomes for each emissions scenario. The CBCCSP, in particular, provided access to additional scenarios and downscaling methods that provided a range of hydrologic outcomes associated with uncertainty in the climate projections, which the WACCIA assessments largely did not. For information on past projects, see our Projects Archive. Building the Columbia Basin-Boundary Region's Capacity to Adapt to Climate Change. The CBCCSP was designed from the outset to support users with a very wide range of technical sophistication and capacity. These extensive and ongoing research activities have also been materially supported by the long-term outreach and education programs of CIG, which have, from the outset, fully recognized the transboundary nature of the CRB (Hamlet, Citation2003; Miles et al., Citation2000) and responded by promoting sustained, long-term interaction with CRB researchers and stakeholders in the United States and Canada (Hamlet, Citation2011). This choice was imposed by WDOE. Originating in British Columbia, it flows 1,214 miles to the Pacific Ocean near Astoria, Oregon. completed or are ongoing in the Columbia River Basin.