columbia basin climate

Lee. Oregon Water Resources Department. Adjusted and Homogenized Canadian Climate Data, British Columbia Ministry of Environment (Canada), Bias Correction and Spatial Disaggregation, Columbia Basin Climate Change Scenarios Project, Composite Delta statistical downscaling method, Climate Impacts Group, University of Washington, Coupled Model Intercomparison Project (Two)Supported the IPCC TAR, Coupled Model Intercomparison Project (Three)Supported the IPCC AR4, Coupled Model Intercomparison Project (Five)Supports the IPCC AR5, A water resources simulation model for the CRB developed by Hamlet and Lettenmaier (, A crop system simulation model developed by Stckle et al. The summary figures for water balance variables at each site have the same format, two examples of which are shown in Fig. 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). The Assessment was initiated in June 2013 and is expected to completed in December 2015. Climate Adaptation. Southwest wind 5 to 15 mph with gusts to around 25 mph. 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. Gridded databases providing full GIS coverage of important hydrometeorological variables in support of a wide range of research applications, including ecosystem research. The methods are discussed in more detail in these references, but a brief description of the procedure is given here to help orient the reader. Also, at about this time, successful lawsuits challenging NEPA studies because they had not addressed climate change effects began to appear (Hamlet, Citation2011). Northeast wind 5 to 10 mph. A key design element of the CBCCSP from the outset of the project was to produce a well-organized and well-documented end-to-end (i.e., GCM to hydrologic products) data processing sequence and a web-accessible data archive that would greatly reduce the cost of producing updates in response to each subsequent CMIP/IPCC cycle. 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). For information on past projects, see our Projects Archive. The Columbia River is the fourth largest river in North America. 2013b. 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. 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).. Although this project consists of an abbreviated set of scenarios and products using three scenarios (high, medium, and low impact) for one downscaling method, the CBCCSP played an important role in providing an established set of methods for developing historical driving datasets and implementing and running the hydrologic models. 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. 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. 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). The largest increases in flooding are in mixed-rain-and-snow basins whose mid-winter temperatures are presently within a few degrees of freezing. 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. 9. Fig. Although results from the WACCIA would arguably have been adequate to support WDOE's adaptation planning, the CBCCSP provided additional foundation support for these efforts, and helped improve confidence in the outcomes of the adaptation strategies identified by better quantifying a range of outcomes. 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. Crook, A. G. (1993). (2010). Littell, J. S., Elsner, M. M., Mauger, G. S., Lutz, E. R., Hamlet, A. F., & Salath, E. P. (2011). The Columbia Basin-Boundary region is already experiencing a climate thats different from 50 years ago. 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. About 10 locations show negative NSE scores, which usually occurs when the simulations are strongly biased in comparison with observations. Funding was received by WSU to carry out research quantifying crop water demand, water resources system performance, and economic impacts under current climate conditions and a range of future climate scenarios. Calibration of the VIC model was carried out using an automated calibration tool called MOCOM-UA developed by the Land Surface Hydrology group at the UW, following the approach described by Yapo, Gupta, and Sorooshian (Citation1998). Figure 1. Yakima River Basin Study 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. 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. (Citation2010) also updated the soil depth map using a more sophisticated approach developed for the DHSVM (Wigmosta, Nijssen, Storck, & Lettenmaier, Citation2002; Wigmosta, Vail, & Lettenmaier, Citation1994) that varies soil depth with elevation. The PET is shown to increase dramatically over most of the domain (primarily because of warming in the scenarios), whereas AET shows widespread declines east of the Cascade Range. 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. About 15 sites in western Washington, outside the CRB, were also included in support of the 2009 WACCIA. (unpublished manuscript). 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. 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. A comprehensive assessment of hydrologic extremes such as Q100 and 7Q10. Changes in PET (PET3, see Table 2) and AET (see Table 2) are shown in Fig. In relatively small basins (approximately 5001500km2), of which there are a substantial number included in the study, errors in meteorological driving data are often a strong determinant of simulation errors. Fig. Recommended articles lists articles that we recommend and is powered by our AI driven recommendation engine. The CBCCSP database has been a valuable resource which has dramatically reduced the cost of a number of high-visibility planning studies in the PNW, including the RMJOC water resources planning studies conducted by the BPA, USBR, and USACE, WSU integrated crop modelling and irrigation water demand studies under HB2860, the WA Integrated Climate Change Response Strategy, and west-wide extensions of the CBCCSP supported by the USFS and USFWS. 7). Both floods (Q100) and extreme 7-day low flows (7Q10) increase in intensity for most of the river sites simulated. From ecosystems, communities, and infrastructure, to our way of lifeeverything will be affected. Other impacts, such as changes in soil moisture dynamics are also apparent in the simulations. %PDF-1.6 % Lows in the upper 40s to lower 50s. 3. 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. (Citation2010) interpolated existing 1/8 degree model parameters to 1/16 degree and also included previously calibrated soil parameters for the Yakima sub-basin (please see acknowledgements). As noted above, the study also supports planning efforts over a wide range of geographic scales. 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). A calibrated 1/16 degree latitude-longitude resolution implementation of the VIC hydrologic model over the Columbia River basin was used to produce historical simulations and 77 future hydrologic projections associated with three different statistical downscaling methods and three future time periods (2020s, 2040s, and 2080s). Rain-dominant basins in the United States (e.g., Chehalis River at Grand Mound in Fig. 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. The multi-model ensemble 30-year mean annual temperature increases by 2.8 C (5.0 C) by late 21st century under RCP4.5 (RCP8.5) over the 1979-1990 baseline, with 18% (24%) more warming in summer. 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. As noted above, such errors are commonly encountered at relatively small spatial scales, particularly when meteorological stations are sparse, and often cannot be resolved using conventional hydrologic model calibration strategies. 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 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. Please note: Selecting permissions does not provide access to the full text of the article, please see our help page The NSE scores for about 20 sites are marginal (between 0.3 and 0.7). The state of Oregon, for example, is classified as about 75% mixed-rain-and-snow for the twentieth century climate. Saturday: Mostly cloudy with a 20 percent chance of rain. The first nine months of the dataset were used for hydrologic model spin-up, resulting in 91 water years (OctoberSeptember) of usable historical data from the hydrologic model simulations. Because of space limitations, we will not be able to cover these alternative modelling efforts in this paper. 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). Twenty-one daily time-step output variables were archived for the VIC simulations (Table 2). Those who wish to do additional post-processing of the existing VIC data can access the archived model output. Naturalized streamflow data were used exclusively in the CBCCSP to calibrate the hydrologic model. The regional report for the National Assessment was supported by two detailed water management studies focused on the CRB by Hamlet and Lettenmaier (Citation1999b) and Miles, Snover, Hamlet, Callahan and Fluharty (Citation2000). Dark red lines show the average of the climate change ensemble. For the BCSD runs (for which the ability to capture key elements of the region's climate variability is arguably even more important to the outcomes) the projections based on the seven highest ranked GCMs (Table 1) were selected for each emissions scenario. 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 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 SRES A1B and B1 GHG emissions scenarios (Nakienovi et al. Each of these methods has its specific advantages and limitations (as discussed in detail in Hamlet et al., 2010a); however, the HD method combines several important strengths of the CD and BCSD methods and was developed specifically to support the prediction of daily hydrologic extremes (Hamlet et al., 2010a). 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. Hamlet, and S.-Y. 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).

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