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Last modified
7/28/2009 2:32:23 PM
Creation date
4/11/2008 3:38:50 PM
Metadata
Fields
Template:
Weather Modification
Contract/Permit #
14-06-D-6467
Title
An Operational Adaptation Program for the Colorado River Basin
Prepared By
Lewis O. Grant, Chappell, Crow, Mielke Jr., Rasmussen, Shobe, Stockwell, Wykstra
Date
10/1/1969
State
CO
Country
United States
Weather Modification - Doc Type
Report
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<br />~ '] <br />~en <br />"'w <br />)-,~5 <br />:.Jz <br />8"" <br />z <br /><t <br />~ <br />o <br />Z <br />w <br />~5 <br />IE <br /> <br />(o ) <br /> <br />(b) <br /> <br />r-- --~PERCENTAGE OF TOTAL SNOWFALL <br />FREQUENCY OF OCCURRENCE <br /> <br />-----, <br />I <br /> <br /> <br />w <br />> <br />~ <br />.J <br />W <br />0:: <br /> <br /> <br />305 310 320 <br />POTENTIAL TEtllf'ERATURE ("I<) <br /> <br />325 <br /> <br />Figure 47. -- (a) Mean Daily Snowfall at Climax as a function of <br />the 700 mb equivalent potential temperature. (b) Distribution <br />of total snowfall and total occurrences as a function of the <br />700 mb equivalent potential temperature computed over a 4- <br />degree class interval. <br /> <br />.J <br />.J <br />tf ID <br />~ <br />Z <br />"'en <br />~~,5 <br />8~ <br /> <br />z <br /><t <br />~ 0 <br />w <br />Cl <br />i:! <br />z <br />w <br />!E5 <br />w <br />a.. <br />w <br />> <br />fi <br />.J <br />W <br />0::0 285 <br /> <br />(01 <br /> <br />{bl <br />FREQ~NCY OF OCCURRENCE <br /> <br />[ENTAGE OF TOTAL <br />SNJWFALL <br />r---- ~ <br />___J I <br />I <br />I <br />I <br /> <br /> <br /> <br />295 300 305 310 315 320 325 <br />EQUIVALENT POTENTIAL TEMFERATURE ("1<) <br /> <br />Figure 48. --(a) Mean Daily Snowfall at Wolf Creek Summit as <br />a function of 700 mb equivalent potential temperature. <br />(b) Distribution of total snowfall and total occurrences as a <br />function of the 700 mb equivalenL poLeIltial temperature <br />computed over a 4-degree class interval. <br /> <br />between 2970 K and 3090 K which contains 53% of a <br />all occurrences. The center of mass is !'it about <br />3010 K. <br /> <br />The mean daily snowfall curve is <br />relatively flat indicating that the equivalent <br />potential temperature explains very little of the <br />variation in the daily snowfal~. This is difficult <br />to reconcile since the adiabat~c condensate <br />increases with the equivalent ~potential tempera- <br />ture, all other effects being equal. It appears <br /> <br />An interesting bi-modal distribution is <br />seen in the snowfall curve with peaks at 2990 K <br />and 3110 K. <br /> <br />58 <br /> <br />r <br /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />--l <br />
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