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This section includes the scope for the entire project which contains tasks performed by <br />the PSC, WWA, CWCB, AwwaRF, and PI(s). <br />Re nest <br />Climate derived weekly streamflow sequences need to be developed for gauging sites <br />important to the study participants (PSC). These new streamflow sequences should be <br />generated from the climate change scenarios and should be representative of two future <br />years of 2040 and 2070. The number and location of these streamflow sites depends on <br />finding and the requirements of the study participants. Streamflow sequences are needed <br />in the upper portions of the Colorado, Arkansas, South Platte, Cache la Poudre, St. Vrain, <br />Boulder Creek„ and Big Thompson River Basins. The PSC further asks that the <br />investigators do a s temperature sensitivity analysis on all basins to verify that the <br />expected results are obtained. <br />Hydrology Models <br />To take advantage of modeling that is already finished or underway, the WEAP (Water <br />Evaluation and Planning) model (developed by the Stockholm Environment Institute) and <br />the Sacramento model (used by the National Weather Service river basin forecast centers) <br />are being considered to convert the climate scenarios to streamflows. Dr. David Yates of <br />NCAR is one of the developers of the WEAP model, and he, along with Colorado <br />Springs Utilities and AwwaRF, is in the process of calibrating that model for the Upper <br />Colorado River Basin down to the Colorado River at Cameo gauging station. If a <br />satisfactory contractual relationship is established with Dr. Yates, he will be asked to <br />calibrate WEAP for the other basins of interest to the project participants (including the <br />Upper Arkansas, Upper South Platte, Big Thompson and Cache la Poudre, St. Vrain, <br />Boulder Creek, Basins). <br />The Sacramento Soil Moisture model is often used in conjunction with the Snow -17 <br />model (also known as the Anderson snow model) to predict streamflow in snowy <br />watersheds based on temperature and precipitation. (Henceforth in this document, the <br />name "Sacramento model" shall mean the linked Snow -17 and Sacramento Soil Moisture <br />models.) The Sacramento model is currently being used by the National Weather Service <br />(NWS) in the Colorado and Missouri River Basins to predict near -term streamflow, and it <br />is already calibrated for significant portions of the Upper Colorado and South Platte <br />River basins. <br />Riverside Technology, a water resources consulting firm in Fort Collins, Colorado, has <br />expertise in the use of the Sacramento model, and has participated in projects to calibrate <br />that model for portions of the Upper Colorado and South Platte River basins. If a <br />satisfactory contractual relationship is established with Riverside Technology, that firm <br />will be asked to calibrate the Sacramento model for the other basins of interest to the <br />project participants. It is believed that better historic natural flow data are available for <br />the South Platte Basin than the data used previously by Riverside in calibrating the <br />model; therefore some recalibration of the South Platte Basin will be necessary. <br />