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points in a basin, and not just at forecast points. A study should be performed to determine if the SNODAS- <br />RDHM system could provide reliable information at internal points in a basin. <br />In the next phase, improvements in snowpack assessment could be achieved by integrating the SNODAS system <br />with forecasting models at CBRFC. CBRFC is in the process of implementing RDHM for the Colorado River. <br />Recent development of historical datasets to drive RDHM allows the models to be calibrated and provides a <br />basis to develop procedures for updating model snow-water-equivalent. Gridded estimates of snow-water- <br />equivalent from CBRFC could be coupled with SNODAS snow-water-equivalent to produce improved volume <br />and spatial estimates of Colorado snowpack. Combining these two estimates will result in improved SNODAS <br />products from NOHRSC and more accurate streamflow forecasts from CBRFC. <br />PHASE III INTERGRATING SNODAS DATA TO FORECAST MODELS <br />In Phase II, RTi investigated using SNODAS data to drive a distributed runoff model. Quantitative use of SNODAS <br />data for snowpack assessment was constrained by a limited period of data availability and volume biases in <br />precipitation inputs to SNODAS. RTi proposes to integrate the SNODAS data with forecasting models at the <br />Colorado Basin River Forecasting Center to address limitations identified in Phase II. RTi plans to use the SWE grids <br />from SNODAS in conjunction with SWE estimates from the CBRFC to generate updated grids that represent the best <br />estimate of snow volume and spatial distribution in selected Colorado basins. Integrating the SWE estimates from <br />SNODAS and CBRFC will result in improved SNODAS products from NOHRSC and more accurate streamflow <br />forecasts. Phase III will also focus on automating snow data processing and display for the State of Colorado. Tools <br />will be developed to process SNODAS and SNOTEL data into maps that can be disseminated to the public. RTi will <br />deliver historical snow data to provide context for current snow conditions. <br />PROJECT OBSTACLES <br />This is a relatively new data source with no historical averages or long data sets to work with. It is a complicated <br />product that will require much analysis to tailor, refine, and develop products that are useful. That being said the daily <br />mapping products are online and water managers can utilize what we have developed so far to track the melt out of <br />snowpack and resulting streamflow. In order to truly use SNODAS operationally and quantitatively water balance <br />budgets and model fixes or correction factors may be warranted for each basin. <br />CONCLUSIONS <br />It is cautioned that the Enhanced Snowpack Assessment Project uses experimental data and should be used <br />provisionally in these early years. Improvements to the model will be made over time and confidence in the output <br />will continue to increase. Water managers have recognized the potential of this project and expressed their support <br />with statements such as: "Could improve the ability to estimate SWE above any particular point such as a reservoir or <br />flood-prone area"; "more detailed than what is currently available"; and "should improve forecasts". There are <br />unprecedented demands on our water resources and it is imperative that we modernize and be able to quantitatively <br />assess the water year and plan accordingly. It is our hope that investment in new technologies and systems like <br />SNODAS will assist us in developing greater certainty in our assessments of SWE, streamflow prediction, and <br />resultant water management decisions. <br />ACKNOWLEDGEMENTS <br />The project is designed to complement Colorado's NRCS Snow Survey's products and not replace them. <br />Indeed, SNOTEL provides critical data to SNODAS. We would like to acknowledge and thank the Colorado NRCS <br />staff members Mike Gillespie, Chris Pacheco, and Thomas Pagano for their assistance in sharing data and insight for <br />the development of the mapping and calculations for this project and commenting on reports. We also would like to <br />the U.S. Bureau of Reclamation, the NWS Office of Hydrologic Development, and Colorado Basin River Forecast <br />Center. Jay Day and his scientific team of Amy Volckens and Michael Thiemann at RTi are commended for their <br />commitment to analyzing and using SNODAS to assist the CWCB with the adaptation of SNODAS for water <br />management objectives. This is amulti-agency collaboration built on the best science available, but is in need of <br />continual change and refinement. Feedback on this applied research project is welcomed and can be directed to the <br />CWCB at joe.busto(a~state.co.us (303) 866-4807, Michelle Garrison at michelle. arrg ison(ae,state.co.us (303) 866 3548. <br />4 <br />