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Last modified
7/28/2009 2:33:38 PM
Creation date
3/20/2008 1:00:24 PM
Metadata
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Template:
Weather Modification
Title
Twelve Basin Investigation - Volume I
Prepared For
Bureau of Reclaimation
Prepared By
Robert D. Elliot, Jack F. Hannaford, Russell W. Chaffer
Date
5/15/1973
Weather Modification - Doc Type
Report
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<br />I <br /> <br />be subject to some depletion or regulation before reaching the downstream gaging <br />stations representing the study watersheds. <br />Estimates of the time-distribution of runoff for each season have been made <br />based upon time-distribution from watersheds typic~l of the massif units. These <br />sub-watersheds represent the massifs in terms of quantity of precipitation, eleva- <br />tion distribution, forest coyer, and other factors apt to influence the time-distri- <br />bution of runoff. Adjustments have been made for precipitation falling outside of <br />\ <br />the October-April seeQ:i.ng_p$r:!-QQ.~d <br />~..... _..--"- <br /> <br />1.3.2 Description of Techni~~. Following is a brief description of techni- <br />ques used in the development of the hydrologic phase of this report. <br />1.3.2.1 Areal distribution of increases in cold orographic precipitation. <br />A technique was required to determine the average and seasonal distribution of the <br />increase in precipitation from seeding cold orographic storms. Meteorologic input <br />was based upon precipitation occurring during the October 1 - April 30 season. ~he <br />areal distribution of incremental precipitation, primarily in the form of sncrwp:~] <br />within massif units has been ~sed =u~n i~ohy~~!_. m~~ _d_~li~~~ting~~~!ra~e October' . <br />1 - April 30 precipit~.tJo!1_. ~' . -~, ' ._~- . <br />1.3.2.2 Physical and hydrologic characteristics. Maps were prepared <br />delineating the various study watersheds within major basin boundaries and the area <br />of effect of the various massif units influencing runoff from the study watersheds. <br />This information was delineated on 1:1,000,000 World Aeronautical Charts and is <br />shown in the Map Appendix. <br />A~~leva.ti~~ata were deve~~~ed for each massif unit by planimetering~ <br />foot contours on the World Aeronautfcal Charts. Where more detail was required, work <br />was done using 1:250,000 Western Untted States Topographic Maps or USGS 15 minute <br />Quadrangles. <br />Maps delineating forested area were used to distinguish forested from alpine <br />regions where runoff characteristics would differ. Generalized soil and geologic <br />maps were utilized as available. <br />Average seasonal (October 1 - April 30) precipitation by elevation zone within <br />,~~c_~_~,:s~if_.~n~t_~a~.d~termined fr.o.~!!...!~?l1ye_!,~l. maps, Although some ~b; ectiv~y <br />entered into evaluation of precipitation by elevation zones, provision was made in <br />the procedure for entry of more than one precipitation quantity if precipitation <br />within the elevation zone and massi:E unit varied considerably. In several instances <br />where October-April isohyetals were not available, average annual isohyetals were <br />used and adjusted for the variation. In some west coast basins, October-April <br /> <br />l <br /> <br />1-41 <br /> <br />I <br />
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