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July temperatures hover in the 90s, with several afternoons during the summer pushing the thermometer reading as high as 100 to 105 degrees. Mostly cloudy, with a high . Lows in the upper 40s to lower 50s. The study is intended to support research, vulnerability assessment, long-term planning, and climate change adaptation by the natural resources management community at a range of spatial scales, by users with varying levels of technical expertise. About 10 locations show negative NSE scores, which usually occurs when the simulations are strongly biased in comparison with observations. Nous avons implment une rsolution latitudelongitude calibre 1/16 de degr dans le modle capacit d'infiltration variable (VIC) et avons appliqu dans le modle bassin du fleuve Columbia pour produire des simulations historiques et 77 projections hydrologiques futures correspondant trois mthodes de rduction dchelle statistique et trois priodes futures (les dcennies 2020, 2040 et 2080). The Hot and the Cold of It Summer comes on strong. Weather for Monday, Feb. 27. Fig. 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. The primary activities and objectives of the RMJOC studies are described in the Executive Summary of the project report (US Department of the Interior, Citation2012): The Bonneville Power Administration (BPA), U.S. Army Corps of Engineers (USACE), and U.S. Bureau of Reclamation (Reclamation) collaborated to adopt climate change and hydrology datasets for their longer-term planning activities in the ColumbiaSnake River Basin (CSRB). Schnorbus, M. A., Bennett, K. E., Werner, A. T., & Berland, A. J. For information on past projects, see our Projects Archive. 2), for which overall errors in meteorological driving data were assumed to be relatively small; then, using these model parameters, to check the results in smaller sub-catchments. 10 Left panel: Changes in Q100 for 297 streamflow locations expressed as a ratio of Q100 for the future period to Q100 for the historical period based on the average of the nine or ten HD scenarios for the B1 and A1B emissions scenarios for three future time periods. Multi-Objective Complex Evolution Procedure, developed at the University of Arizona (Yapo et al., A water resources simulation model developed by Labadie (, National Centers for Environmental Prediction, Pacific Climate Impacts Consortium, University of Victoria. These products are available for all 77 climate scenarios listed in Table 1, as well as for the historical simulation. 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. 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). . This study represents one of the first attempts to dynamically couple a sophisticated, physically based hydrologic model with a detailed crop model to estimate the integrated impacts on water supply and crop viability at a range of spatial scales. One of the first major efforts of CIG in this area was focused on the preparation of a detailed and comprehensive regional assessment report for the PNW for the 1999 National Assessment of the Impacts of Climate Variability and Change in the United States (ultimately published as Mote et al., Citation2003). A remote sensing approach, The NorWeST Summer Stream Temperature Model and Scenarios for the Western U.S.: A Crowd-Sourced Database and New Geospatial Tools Foster a User Community and Predict Broad Climate Warming of Rivers and Streams, The coastal streamflow flux in the Regional Arctic System Model, Tidal-Fluvial and Estuarine Processes in the Lower Columbia River: II. 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. In much of the CRB, however, summer AET is water limited (i.e., there is abundant surface energy to evaporate whatever water is available), and changes in AET are dominated by decreasing summer precipitation in the scenarios, which effectively decreases summer AET in most cases. Each of the six panels in the figure shows the long-term monthly mean for the 10 (9 for B1) HD GCM scenarios (red lines) and the historical simulations (blue lines). Please note: Selecting permissions does not provide access to the full text of the article, please see our help page Source: 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). Gusts up to 20 mph in the morning. 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. This approach was partly based on practical limitations on time and computational resources but was also informed by previous experience using the VIC model at finer spatial scales. Key products from the study include detailed summary data for about 300 river sites in the PNW and monthly GIS products for 21 hydrologic variables over the entire study domain. 2013b. Three statistical downscaling approaches were selected or developed for the study: Composite Delta (CD): regional average projections compiled from 10 GCMs (Elsner et al., Citation2010), Bias Correction and Spatial Downscaling (BCSD): (Salath, Citation2005; Salath, Mote, & Wiley, Citation2007; Wood, Leung, Sridhar, & Lettenmaier, Citation2004; Wood, Maurer, Kumar, & Lettenmaier, Citation2002), Hybrid Delta (HD): (Hamlet et al., 2010a). Building the Columbia Basin-Boundary Region's Capacity to Adapt to Climate Change. Highs in the lower to mid 40s. The choice of the A1B scenario, however, was informed by the authors viewpoint that this scenario is an instructive and plausible scenario reflecting relatively little GHG mitigation until mid-century (similar to A2 until about 2050), followed by more effective GHG mitigation efforts in the second half of the twenty-first century as impacts intensify. Fig. Highs in the lower to mid 60s. (unpublished manuscript). The magnitude of hydrologic extremes such as Q100 and 7Q10 are expected to shift markedly in some basins in response to cool season warming, increasing cool season precipitation, and warmer, drier summers. Over the last several years, the USFS and USFWS have engaged with the CIG to produce a set of initial climate change hydrologic scenarios over much of the west using a common methodology intended to support landscape-scale assessment of climate change impacts (Littell et al., Citation2011). Act relating to water resource management in the Columbia river basin, H.R. As a result the largest changes in snowpack are apparent in the simulations for relatively warm coastal mountain ranges, such as the Cascade Range, and at moderate elevation in the Rockies, where snowpack is most sensitive to changes in temperature of a few degrees Celsius. Fig. It drains roughly 260,000 square miles and travels more than 1,240 miles from its headwaters in the Rocky Mountains to its confluence with the Pacific Ocean. Determining surface water availability in Oregon. 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. This was coordinated through the River Management Joint Operating Committee (RMJOC), a sub-committee of the Joint Operating Committee which was established through direct funding Memorandum of Agreements between BPA, Reclamation, and the USACE. Building the Columbia Basin-Boundary Region's Capacity to Adapt to Climate Change. The smallest of these sub-basins is about 500km2 (approximately fifteen 1/16 degree VIC cells), and the largest encompasses most of the CRB (approximately 620,000km2 or about 18,800 VIC cells). At the other extreme, for those without any hydrologic modelling or post-processing capability the study provides a wide range of hydrologic products that can be used without any expertise in the preceding steps. In the first five years (19952000) of operation, the research efforts of CIG were primarily directed towards the assessment of the impacts of interannual and interdecadal climate variability associated with ENSO (Battisti & Sarachik, Citation1995; Trenberth, Citation1997) and the PDO (Gershunov & Barnett, Citation1998; Mantua, Hare, Zhang, Wallace, & Francis, Citation1997). These results point to extensive, landscape-scale transformations in hydrologic behaviour associated with climate change. In 2008, many of the financial and institutional barriers to climate change assessment and adaptation that had been erected over the preceding eight years by the Bush Administration were substantially reduced by the incoming Obama Administration. As mentioned above, 20062007 was something of a turning point for regional stakeholders considering future actions to prepare for climate change. Implications of global climate change for snowmelt hydrology in the 21st century, Modeling snow accumulation and ablation processes in forested environments, Uncertainties in hydrologic and climate change impact analyses in headwater basins of British Columbia. Preparing for climatic change: The water, salmon, and forests of the Pacific Northwest. Even with substantial cuts to greenhouse gas emissions, scientists expect our climate to continue changing over the coming decades. 2 Eleven sub-basins in the CRB used for large scale calibration (left panel). Increasing low flow risks (declining 7Q10 values) are widespread across the domain as a result of the combined effects of declining snowpack (which tends to result in earlier streamflow recession and lower flows in late summer, see Fig. In addition to creating these datasets, the RMJOC agencies worked together to adopt a set of methods for incorporating these data into those longer-term planning activities. An overview of the Columbia Basin Climate Change Scenarios Project: Approach, methods, and summary of key results. About 50 of the 80 sites evaluated show monthly NSE scores greater than or equal to approximately 0.7 (good to excellent fit). 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). 7). In addition, some observed streamflow data are suitable for use as natural data if the effects of storage and diversions are relatively small (e.g., for the USGS Hydro-Climatic Data Network streamflow sites). Using the VIC model, Mote, Hamlet, Clark, and Lettenmaier (Citation2005), Mote, Hamlet, and Salath (Citation2008), for example, showed excellent reproduction of observed trends in 1 April SWE over both the PNW as a whole and over the Cascade Range in Oregon and Washington. 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). The CBCCSP was developed to address these diverse needs. This has prompted the National Weather Service to issue a winter weather advisory for the Tri-Cities, Walla Walla, Hermiston, and surrounding areas in effect from 04:00 to 22:00 Sunday. 95 0 obj <> endobj Nakienovi, N., Alcamo, J., Davis, G., De Vries, B., Fenhann, J., Gaffin, S.,Dadi, Z. 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. However, our goal in this case was not to reduce the range of uncertainty by selecting a smaller group of GCMs. (Citation2010) over the entire PNW (Tohver et al. What Matters Most: Are Future Stream Temperatures More Sensitive to Changing Air Temperatures, Discharge, or Riparian Vegetation? During the study (and afterwards), some stakeholders expressed interest in including less optimistic emissions scenarios (such as SRES A1FI), in order to better understand the implications of a potential worst case scenario. Highs in the lower 80s. REVEL=Columbia River at Revelstoke Dam, CORRA=Kootenay River at Corra Linn Dam, WANET=Pend Oreille River at Waneta Dam, LIBBY=Kootenai (Kootenay) River at Libby Dam, DWORS=N. Fork Clearwater River at Dworshak Dam, MILNE=Snake River at Milner, ICEHA=Snake River at Ice Harbor Dam, PRIRA=Columbia River at Priest Rapids Dam, YAPAR=Yakima River at Parker, DALLE=Columbia River at The Dalles, OR, WILFA=Willamette River above falls at Oregon City. Because of a general lack of observed naturalized daily time-step flow for most streamflow sites, daily time step calibration using additional parameters such as the infiltration parameter (bi ) in VIC (Liang et al., Citation1994), or routing parameters (such as the unit hydrograph for each cell) were not attempted during the study. 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. Figure 4 shows a flow chart of these post-processing steps. These include the full meteorological forcings for the model (variables 18), a suite of water balance variables simulated by the model (variables 916), and five different PET metrics (variables 1721) (Elsner et al., Citation2010). Hydrologic sensitivity of global rivers to climate change. Has spring snowpack declined in the Washington Cascades? Cooper, R. M. (2002). Casola, J. H., Kay, J. E., Snover, A. K., Norheim, R. A., Binder, L. C. W., & the Climate Impacts Group. A detailed climate change assessment report was prepared by the CIG for Seattle City Light (Snover et al., Citation2010) based primarily on the CBCCSP database. (Citation2010). Hamlet, and S.-Y. These approaches are also useful for avoiding biases in the streamflow simulations that result from systematic errors in gridded precipitation or temperature data. The Assessment will result in a better understanding the potential impacts of climate change on the eight components identified in SECURE in the Columbia River Basin. A family of greenhouse gas emissions scenarios used in the IPCC effort (Nakienovi et al. These annual peak daily flows are then ranked and assigned a quantile value using an unbiased quantile estimator based on the method of Cunane (Stedinger, Vogel, & Foufoula-Georgiou, Citation1993). Extreme event statistics are calculated directly from the raw (i.e., not bias-adjusted) daily streamflows at each streamflow site, applying methods developed by Hamlet and Lettenmaier (Citation2007) and Mantua et al. 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. Depending on their needs and/or level of technical sophistication, users can tap into the study databases at a number of different levels. Originating in British Columbia, it flows 1,214 miles to the Pacific Ocean near Astoria, Oregon. Detailed forecast for Lower Columbia Basin of Washington Rest Of Today Partly sunny. Fig. Bias adjustment was also used in preparing the specific reservoir modelling support products discussed below. They found that the vast majority of locations across the Columbia River Basin are expected to experience increases in maximum streamflow magnitudes in the future. %%EOF These parameters were chosen because they strongly affect the timing and volume of runoff production in the model simulations and are, in general, not available from observed data. By late 21st century, annual precipitation increases by 5% (8%), with an 8% (14%) winter increase and a 4% (10%) summer decrease, but because . 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). 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. 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. Lee. hb```"V* aB@{= ,!It#GjWeyP1% Although not as extreme as A1FI, the high-end A2 scenario was archived by most GCMs and could have been used in the CBCCSP in place of the A1B scenario.

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columbia basin climate