columbia basin climate

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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. The objective function for the optimization process in this case was: where Q is the monthly streamflow; NSE(Q) is the NSE (monthly flow), which varies between [inf, 1] and typically between [0,1]; NSE(log(Q+1)) is the NSE (monthly flow), which varies between [inf, 1] (this metric places less emphasis on high flow errors in calculating NSE); Vol_Err(Q) is the annual volume error (in 1000 acre feet); R 2(Q)=R 2 (squared correlation coefficient between simulated and observed Q), which varies between [0,1]; Peak_Diff(Q) is the mean hydrograph peak differencethe absolute value varies for different sites; RMSE(Q) is the root mean square error, whose absolute value varies for different sites; and NumSC(Q) is the number of sign changes in the errors (this metric penalizes simulations with too much month-to-month variability in comparison with observations). Here we will review a few important aspects of the basic implementation to help orient the reader and will then focus most of our attention on the additional implementation and calibration tasks carried out during the CBCCSP. Glacier outlines are automatically generated from satellite imagery and are provided by, Species and Ecosystems at Risk as identified by the, Current bioclimates and modeled bioclimates for three future climate scenarios in 2080s. The Columbia Basin Climate Source is your one-stop destination for information about climate change, impacts, and action in this region. The WDOE was also directed to incorporate climate change explicitly in these comprehensive assessment efforts. 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. 6 Example of a summary plot for extreme high flows (Q20, Q50, Q100, left panels) and extreme low flows (7Q10, right panels) for the Skagit River at Mount Vernon for two emissions scenarios (A1B, B1) and three future time periods (2020s, 2040s, 2080s). completed or are ongoing in the Columbia River Basin. 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 Columbia Basin-Boundary region is already experiencing a climate that's different from 50 years ago. Lee. 135 0 obj <>stream The data is accessible for decision makers, researchers, students, professionals and the public. Lee. 7 Left panel: Simulated historical 1 April snow water equivalent (SWE) (upper right) and percentage changes in 1 April SWE for two emissions scenarios and three future time periods extracted from the CD VIC scenarios. Changes in PET (PET3, see Table 2) and AET (see Table 2) are shown in Fig. Thus, stakeholders can select different products, using different downscaling approaches that are appropriate to their needs. Associated shifts in streamflow timing from spring and summer to winter are also evident in basins that currently have significant snow accumulation in winter, whereas rain-dominant basins show minimal shifts in streamflow timing. 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). Additional meteorological forcings needed for hydrologic model simulations (e.g., net incoming long- and shortwave radiation, dew point temperature, etc.) 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). This is a good example of the use of the study data to support relatively fine-scale planning needs. Fig. Three VIC model calibration parameters described above were varied in the optimization process, and six error metrics were used to define the objective function: squared correlation coefficient (R 2), NSE, the NSE of log-transformed data, annual volume error, mean hydrograph peak difference, RMSE, and number of sign changes in the simulated streamflow errors. Columbia Basin Water Hub - Living Lakes Canada Blue lines show the average historical values (19162006) (repeated in each panel). Weather for Queens Cup Basin, British Columbia, Canada 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. These data are summarized in figures and tables prepared for each streamflow site discussed in Section 4. 2013. This daily disaggregation technique sometimes introduces an undesirable discontinuity in the bias-corrected daily values at the beginning and end of months. 1990 level modified streamflow 19281989. Columbia Basin | WA - DNR 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). Originating in British Columbia, it flows 1,214 miles to the Pacific Ocean near Astoria, Oregon. John Day basin century climate change: +1.5 degF day temperature, +3.2 degF night temperature, -0.4 inch (2%) less precipitation. 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. Fig. Columbia Basin Care Explore the basics of climate science arrow . We use cookies to improve your website experience. Bias adjustment was also used in preparing the specific reservoir modelling support products discussed below. A flight of geese circle over Moses Lake Saturday morning. Detailed forecast for Lower Columbia Basin of Washington Rest Of Today Partly sunny. Previso do tempo local de hora em hora, condies climticas, precipitao, ponto de condensao, umidade, vento no Weather.com e The Weather Channel Evidence includes increases in global average air and ocean temperatures, widespread melting of snow and ice, and rising global mean sea level. During initial model development steps, Elsner et al. 8) experience little change in the shape of the monthly hydrograph because there is only occasional low-elevation snow in mid-winter in the twentieth century base case; therefore, there is relatively little sensitivity of monthly runoff timing to warming. Ingalls Weather - Weather reports on whatever I decide to report on. (For example, Dworshak and Milner are nested within the larger Ice Harbor sub-basin.). 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. 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 top two panels show the Nash Sutcliffe Efficiency (NSE) (left) and R 2 (right) for the calibration period, while the two lower panels show NSE (left) and R 2 (right) for the validation period. As an integrated priority, the Trust has integrated climate resilience into its strategic priorities by supporting: wildfire risk reduction and job creation through the Columbia Basin Wildfire Resiliency Initiative energy retrofits, repairs and alternative energy generation at community-purpose buildings through the Non-profit Sustainability - Building Support Grants 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. 12 Changes in monthly mean total column soil moisture (OctoberSeptember) for three representative river sites in the PNW: Kootenay River at Corra Linn Dam (left), Columbia River at The Dalles, Oregon (centre), and Yakima River at Parker (right). (2011). Climate Change Impacts on the Columbia Basin Typical month of historical flooding events is shown by the colour of the dots in the scatter plot (legend inset in the upper right corner), by permission of I. Tohver, A.F. The changes in the importance of snow in some areas of the United States are particularly striking. Starting from these parameter sets, an additional large-scale calibration was performed during the CBCCSP to improve model performance in reproducing historical streamflow. (unpublished manuscript). Fig. Citation2000) were selected as the basis for the study because they provide a) a wide range of plausible outcomes while also reflecting some potential GHG mitigation by the end of the twenty-first century, and b) most of the approximately 20 GCM projections associated with the CMIP3 archived runs from both emission scenarios (Mote & Salath, Citation2010). Data from the CBCCSP are currently supporting two CIG studies funded by the LCCs and the CSC, including a study of impacts to wetlands in the PNW (funded by the North Pacific LCC and the PNWCSC) and a study assessing climatic and hydrologic extremes and their effects on ecosystems over the western United States (funded by the PNWCSC). 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. The interested reader is directed to the CBCCSP report (Hamlet, Carrasco, et al., Citation2010a, Chapter 6) for a detailed discussion of methods and results. A set of simpler, lumped-storage reservoir operations models was used to quantify impacts in a number of smaller water supply systems. Gusts up to 20 mph in the morning. The approach used a refined version of the methods established by Hamlet and Lettenmaier (Citation2005), which created a hybrid historical meteorological dataset based on three primary data resources: a) monthly HCN data in the United States and the similar AHCCD datasets in Canada, b) daily data from the cooperative station network in the United States (co-op stations) and similar data from Environment Canada, and c) a monthly climatology (19712000) for precipitation and daily minimum and maximum temperatures at 30 arc-second resolution produced using the PRISM (Daly, Gibson, Taylor, Johnson, & Pasteris, Citation2002; Daly, Neilson, & Phillips, Citation1994; DiLuzio, Johnson, Daly, Eischeid, & Arnold, Citation2008).



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