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WSPC03871
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Last modified
1/26/2010 11:36:38 AM
Creation date
10/9/2006 4:14:31 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8200.700
Description
Colorado River Basin General Publications - Augmentation-Weather Modification
State
CO
Basin
Colorado Mainstem
Water Division
5
Date
3/1/1979
Author
DOI-BOR
Title
Project Skywater - Fiscal Years 1975-78 Report - Atmospheric Resources Management Program
Water Supply Pro - Doc Type
Report/Study
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<br />00257~ <br /> <br />CONTRACTOR: Amos Eddy, Inc., Norman, Oklahoma <br />CONTRACT NO. 6-07-DR-20050 <br />PRINCIPAL INVESTIGATOR: Amos Eddy <br />PERIOD: December 1, 1975, to February 1, 1977 <br />FUNDING: FY76 - $9,683 <br />T.Q. - $3,683 <br /> <br />This study provided an optimal sampling objective analysis and <br />processed data display for the HIPLEX design. <br /> <br />Principal findings are: <br /> <br />(1) Surface rain gage data can be combined with radar reflec- <br />tivity data to analyze the total surface rainfall within objec- <br />tively determined confidence limits. <br /> <br />(2) A limi'ted gage network, more sparse than that required to <br />produce a satisfactory independent analysis but adequate to <br />"calibrate" the radar reflectivities, can be defined. This in <br />turn, produces a satisfactory analysis of surface total rainfall. <br /> <br />(3) Evidence confirms that patterns of rainfall are provided by <br />the radar data while the magnitudes are measured by the gage <br />data. <br /> <br />(4) The covariance function climatology will give a strong <br />indication of the preferred sensor deployment along and across the <br />storm motion. <br /> <br />(5) The marginal increase in analysis accuracy as the surface <br />gage density is increased is shown (a) for the case when no radar <br />data are available and (b) for the case when radar data are <br />available. <br /> <br />(6) Analysis of variance results indicates that the attentuation <br />associated with the 5-cm radar data used is considerably less than <br />that caused by other vari ables in an "average" storm, but could <br />have a considerable effect on the objective analysis estimate of <br />rain "behind" the heavy rainstorms. <br /> <br />II 1-24 <br />
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