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Last modified
7/28/2009 2:42:09 PM
Creation date
4/30/2008 2:44:24 PM
Metadata
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Template:
Weather Modification
Contract/Permit #
14-06-D-7052
Title
Ecological Impacts of Snowpack Augmentation in the San Juan Mountains, Colorado
Date
3/1/1976
State
CO
Weather Modification - Doc Type
Report
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<br />Table 8. Spring precipitation (April, May) <br />Synoptic Percent of Days <br />Type Type Occurs <br />20 17 <br />110 6 <br />111 8 <br />120 18 <br />210 6 <br />211 1 <br />220 12 <br />230 4 <br />320 11 <br />321 1 <br />330 12 <br />331 4 <br /> TOTAL 100 <br />Main types responsible for precipitation in spring months: <br /> <br /> % of Total Spring Precipitation <br />a) Durango b) Silver ton <br /> 15.9 18.7 <br /> 3.4 5.8 <br /> 9.0 8.4 <br /> 26.9 25.1 <br /> 1.8 2.7 <br /> 1.2 0.4 <br /> 11.1 11.3 <br /> 4.0 2.2 <br /> 14.9 15.1 <br /> 1.9 1.0 <br /> 7.0 7.3 <br /> 3.0 2.0 <br /> 100 100 <br /> <br />20 (B) <br />120 (A) 69% of precipitation at Durango <br />220 (Bn_c) 70% of precipitation at Silverton <br />320 (Em) <br /> <br />These four types occurred on 58% of days from 1928 to 1958. <br /> <br />in summer months in relation to summer precipi- <br />tation totals at Durango. Once again, while in the <br />early 1930's there is a general positive relation- <br />ship between above normal precipitation and above <br />normal type frequency, the relationship after that <br />is almost inverse. The reasons for such a poor <br /> <br />correspondence between the type of frequency on a <br />season-to-season basis, and seasonal precipitation <br />totals presumably reflect high variability within <br />types. Whereas the main types may occur on nearly <br />all days in a season (e.g. 1945), precipitation <br />totals may remain low due to particularly dominant <br />small-scale synoptic situations within each major <br />synoptic' type. <br /> <br />Table 9. Summer precipitation (June, July, August) <br /> <br />Synoptic Percent of Days <br />Type Type Occurs <br />20 (B) 22.1 <br />110 (Bn_a) 18.8 <br />111 (Bn_b) 2.7 <br />120 (A) 29.3 <br />210 (F/CL) 0.9 <br />220 (B ) 11.7 <br /> n-c <br />230 (D) 9.2 <br />320 (Em) 1.9 <br />330 (EL) 3.0 <br />. 331 (En) 0.3 <br /> TOTAL 100 <br />Main types responsible for precipitation in summer months: <br /> <br />% of Total Summer Precipitation <br />a) Durango b) Silver ton <br /> <br />26.5 24.6 <br />15.0 20.0 <br />1.1 1.7 <br />31.2 27.6 <br />0.7 0.6 <br />14.7 13.8 j <br />7.0 8.7 1 <br />1.0 0.3 <br />2.8 2.6 'I <br /> , <br />0.0 0.0 ',' <br />100 100 <br /> <br />20 <br /> <br />110 <br />120 <br /> <br />(B) <br />(Bn_) <br />(A) <br /> <br />73% of precipitation at Durango <br />72% of precipitation at Silver ton <br /> <br />The three types occurred on 70% of days from 1928 to 1958. <br /> <br />62 <br /> <br />( <br /> <br />," <br />
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