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<br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br />. <br /> <br />EXECUTIVE SUMMARY <br /> <br />The Colorado Weather Damage Modification Program (WDMP) research <br />project involved a physical evaluation of the Denver Water (DW) operational <br />winter orographic cloud seeding program in the central Colorado Rockies for the <br />winter season 2003-2004 using the Colorado State University mesoscale <br />Regional Atmospheric Modeling System (RAMS). The project was piggy-backed <br />onto the DW operational program contracted by Western Water Consultants <br />(WWC), LLC. The target area was the Blue, Upper Blue, Snake, Williams Fork, <br />and Upper South Platte River drainage basins above 9,000 feet elevation (see <br />Figure 2.1). The area within the target boundary was about 3,700 km2. From <br />February 10 through March 2004 only the Upper South Platte River basin and <br />along the Continental Divide above the Upper Blue River basin was to be <br />targeted. Using a finest grid spacing of 3-km, RAMS was run first in real-time to <br />provide operational support to the DW cloud seeding program. RAMS was <br />subsequently rerun for the period of operations with a number of improvements <br />derived from assessments of the real-time runs, and then rerun with simulated <br />seeding generators releasing seeding material (Agl) at rates, time periods, and <br />locations consistent with the operational program. <br /> <br />As a mesoscale model, RAMS is unique in its ability to explicitly represent <br />the activation of cloud nucleating aerosols (CCN and IN) including seeded IN, to <br />simulate the transport and dispersion of seeding material, the explicit nucleation <br />and vapor deposition, riming, and aggregation growth of ice particles, and <br />amounts and types of precipitation. Moreover, it was able to do so for an entire <br />operational cloud seeding program. We believe that this project establishes a <br />"model" of a methodology for physical and statistical evaluation of future seeding <br />projects. However, it must be recognized that this was a first prototype model <br />and as such things did not work out entirely according to our expectations. <br /> <br />The major results of this research project are as follows: <br /> <br />. WWC (Larry Hjermstad) found that after the model fixes had been <br />implemented in mid-February 2004 and the RAMS real-time forecast 0000 <br />UTC cycle was run on the new PC cluster, the forecast output that was <br />posted on the Web site was very useful. The low-level warm temperature <br />problem had been greatly reduced and the model provided timely input for <br />operational cloud seeding decision making. There were numerous <br />forecast products and parameters to evaluate. In addition to the 2-hr <br />forecast presentations, the animated forecast loops provided a quick <br />visual picture of changes over time. <br />. Larry Hjermstad did point out the forecast model exhibited a warm <br />temperature bias at 700 mb which reduced its effectiveness as a decision <br />tool for determining if seeding operations should proceed. Causes of the <br />warm bias were determined and fixes were made in mid-February 2004. <br />The entire winter season was re-run to provide a better estimate of natural <br /> <br />xv <br />