Mitigating the Effects of Climate Change on the Water Resources of the Columbia River Basin

The potential effects of climate change on the hydrology and water resources of the Columbia River Basin (CRB) were evaluated using simulations from the U.S. Department of Energy and National Center for Atmospheric Research Parallel Climate Model (DOE/NCAR PCM). This study focuses on three climate projections for the 21st century based on a `business as usual' (BAU) global emissions scenario, evaluated with respect to a control climate scenario based on static 1995 emissions. Time-varying monthly PCM temperature and precipitation changes were statistically downscaled and temporally disaggregated to produce daily forcings that drove a macro-scale hydrologic simulation model of the Columbia River basin at 1/4-degree spatial resolution. For comparison with the direct statistical downscaling approach, a dynamical downscaling approach using a regional climate model (RCM) was also used to derive hydrologic model forcings for 20-year subsets from the PCM control climate (1995–2015) scenario and from the three BAU climate(2040–2060) projections. The statistically downscaled PCM scenario results were assessed for three analysis periods (denoted Periods 1–3: 2010–2039,2040–2069, 2070–2098) in which changes in annual average temperature were +0.5,+1.3 and +2.1 °C, respectively, while critical winter season precipitation changes were –3, +5 and +1 percent. For RCM, the predicted temperature change for the 2040–2060 period was +1.2 °C and the average winter precipitation change was –3 percent, relative to the RCM controlclimate. Due to the modest changes in winter precipitation, temperature changes dominated the simulated hydrologic effects by reducing winter snow accumulation, thus shifting summer streamflow to the winter. The hydrologic changes caused increased competition for reservoir storage between firm hydropower and instream flow targets developed pursuant to the Endangered Species Act listing of Columbia River salmonids. We examined several alternative reservoir operating policies designed to mitigate reservoir system performance losses. In general, the combination of earlier reservoir refill with greater storage allocations for instream flow targets mitigated some of the negative impacts to flow, but only with significant losses in firm hydropower production (ranging from –9 percent in Period1 to –35 percent for RCM). Simulated hydropower revenue changes were lessthan 5 percent for all scenarios, however, primarily due to small changes inannual runoff.

[1]  D. Lettenmaier,et al.  A simple hydrologically based model of land surface water and energy fluxes for general circulation models , 1994 .

[2]  C. Brooks Climatic Change , 1913, Nature.

[3]  Xindi Bian,et al.  Mid-Century Ensemble Regional Climate Change Scenarios for the Western United States , 2004 .

[4]  Richard N. Palmer,et al.  Potential Implications of PCM Climate Change Scenarios for Sacramento–San Joaquin River Basin Hydrology and Water Resources , 2004 .

[5]  Dennis P. Lettenmaier,et al.  Hydrologic sensitivities of the Sacramento‐San Joaquin River Basin, California, to global warming , 1990 .

[6]  D. Lettenmaier,et al.  Streamflow simulation for continental‐scale river basins , 1997 .

[7]  G. McCabe,et al.  GENERAL‐CIRCULATION‐MODEL SIMULATIONS OF FUTURE SNOWPACK IN THE WESTERN UNITED STATES 1 , 1999 .

[8]  James W. Hurrell,et al.  Elevation Dependency of the Surface Climate Change Signal: A Model Study , 1997 .

[9]  W. G. Strand,et al.  The ACPI Climate Change Simulations , 2004 .

[10]  Arun Kumar,et al.  Long‐range experimental hydrologic forecasting for the eastern United States , 2002 .

[11]  Dennis P. Lettenmaier,et al.  EFFECTS OF CLIMATE CHANGE ON HYDROLOGY AND WATER RESOURCES IN THE COLUMBIA RIVER BASIN 1 , 1999 .

[12]  J. Houghton,et al.  Climate change 2001 : the scientific basis , 2001 .

[13]  Y. Qian,et al.  Hydroclimate of the Western United States Based on Observations and Regional Climate Simulation of 1981–2000. Part I: Seasonal Statistics , 2003 .

[14]  Alan F. Hamlet,et al.  PACIFIC NORTHWEST REGIONAL ASSESSMENT: THE IMPACTS OF CLIMATE VARIABILITY AND CLIMATE CHANGE ON THE WATER RESOURCES OF THE COLUMBIA RIVER BASIN 1 , 2000 .

[15]  T. Barnett,et al.  The ACPI Project, Element 1: Initializing a Coupled Climate Model from Observed Conditions , 2004 .

[16]  L. Vail,et al.  Sensitivity of Pacific Northwest Water Resources to Global Warming , 2005 .

[17]  T. Barnett,et al.  Detection of Anthropogenic Climate Change in the World's Oceans , 2001, Science.

[18]  D. Lettenmaier,et al.  Hydrologic Sensitivity of Global Rivers to Climate Change , 2001 .

[19]  W. G. Strand,et al.  Parallel climate model (PCM) control and transient simulations , 2000 .

[20]  D. Lettenmaier,et al.  Hydrologic Implications of Dynamical and Statistical Approaches to Downscaling Climate Model Outputs , 2004 .

[21]  D. Lettenmaier,et al.  The Effects of Climate Change on the Hydrology and Water Resources of the Colorado River Basin , 2004 .

[22]  Dennis P. Lettenmaier,et al.  Long range experimental hydrologic forecasting for the eastern U.S. , 2002 .

[23]  Dennis P. Lettenmaier,et al.  Economic Value of Long-Lead Streamflow Forecasts for Columbia River Hydropower , 2002 .

[24]  Dennis P. Lettenmaier,et al.  Climatic Sensitivity of California Water Resources , 1991 .

[25]  D. Lettenmaier,et al.  A Long-Term Hydrologically Based Dataset of Land Surface Fluxes and States for the Conterminous United States* , 2002 .

[26]  S. Ghan,et al.  Parameterizing Subgrid Orographic Precipitation and Surface Cover in Climate Models , 1998 .

[27]  Elizabeth L. Chalecki,et al.  THE IMPACTS OF CLIMATIC CHANGES FOR WATER RESOURCES OF THE COLORADO AND SACRAMENTO‐SAN JOAQUIN RIVER BASINS 1 , 1999 .

[28]  Richard N. Palmer,et al.  Water Resources Implications of Global Warming: A U.S. Regional Perspective , 1999 .

[29]  S. Ghan,et al.  Pacific Northwest Climate Sensitivity Simulated by a Regional Climate Model Driven by a GCM. Part I: Control Simulations , 1999 .