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Last modified
7/28/2009 2:29:00 PM
Creation date
1/17/2007 2:20:14 PM
Metadata
Fields
Template:
Weather Modification
Applicant
CWCB
Sponsor Name
USBR
Project Name
Response to RFP
Title
Numerical Simulations of Snowpack Augmentation for Drought Mitigation Studies in the Colorado Rocky Mountains
Prepared For
USBR
Prepared By
Joe Busto, CWCB
Date
8/20/2003
Weather Modification - Doc Type
Application
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<br />- <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />II <br /> <br />More recent cases in which ETA upper air and surface analysis data plus ETA soil <br />moisture data provide the best agreement with observations. <br /> <br />. Even in cases where the maximum simulated precipitation amounts are in close <br />agreement with observations, the actual scenario of convective evolution is often <br />different from that observed. In other words, owing to the inability of upper air, <br />and surface data, as well as land-surface parameters (especially soil moisture) to <br />represent completely the real world, the model climatology differs from actual <br />climatology. These data are more poorly observed in the older convective cases so <br />that the model climatology of those events varies more from the observed storm <br />behavior, than in the more recent storms. <br /> <br />. Sensitivity tests reveal that simulations of heavy convective events are highly <br />sensitive to the specification of initial soil moisture fields. <br /> <br />. Precipitation maxima occurring at higher elevations have significant contributions <br />from hail, which reduces surface runoff rates due to prolonged melting. <br /> <br />The PMP estimates that we have made should be viewed as a demonstration of concept <br />only. The data used for our estimates are too limited to provide useful quantitative PMP <br />estimates. We had to limit our analysis to recent storms because we found that the NCEP <br />reanalysis data were inadequate for the purpose of extreme precipitation simulations. <br />Higher resolution ETA-based reanalysis data may overcome this deficiency and permit <br />more reliable PMP estimates in the future. <br /> <br />3) Contact person for this project would be: <br /> <br />Mr. Jack Byers, Asst. State Engineer <br />Dept. of Natural Resources <br />Division of Water Resources <br />1313 Sherman Street, Rm. 818 <br />Denver, CO 80203 <br />(303) 866-3581 <br /> <br />8.2 CWCB and WWC <br /> <br />Please see Section 6.2 on page 25 in this Technical Proposal. <br /> <br />II -40 <br />
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