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Last modified
7/28/2009 2:37:26 PM
Creation date
4/16/2008 10:37:01 AM
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Template:
Weather Modification
Contract/Permit #
14-06-D-7659
Title
Weather Modification Design Study for Streamflow Augmentation in the Northern Sierra Nevada
Date
7/1/1976
Weather Modification - Doc Type
Report
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<br />_~'l:i...o-" <br /> <br />is desirable or would be detrimental. Suspension rules governing seeding <br />operations are given in Volume III. <br /> <br />The reservoirs serve a multitude of purposes, two of <br />which are to provide flood control and to ameliorate the year-to-year <br />pi'ecipitation variability. In this latter capacity; they hold excess <br />run-off from one year to be used in the next. Thus, the effect of <br />seeding to increase run-off in one year can, through the reservoir, be <br />extended to alleviate deficits in a subsequent dry year, but not a previous <br /> <br />one. <br /> <br />Withholding seeding ope rations early in the season <br />results in the risk of missing early opportunities with the possibility <br />of inadequate opportunities being available in the later season. However, <br />this ri?k is relatively small. In fact, model results and data analysis <br />indicate that the m.iddle part of the winter (January and February) are <br />the months of highest potential in most years. This is due both to the <br />frequency of storms over the year and the fact that mid-winter storms <br />are more likely to be snowstorms rather than rain storms. <br /> <br />3.3 <br /> <br />Hydrologic Considerations <br /> <br />The re we re four rec omrnendations in the San Diego State <br />report conce rning hyd rology. These recommendations are listed below <br />with a discussion of the study results relating to them presented in the <br />following paragraphs. <br /> <br />. An analys is, based on existing hydrologic models, <br />should be made of anticipated changes in flow regim.e of several repre- <br />sentative snlaller streams in the Sierra Nevada under alternative snow <br />augmentation strategies. Similar analyses should be made for <br />representative high-elevation lakes and reservoirs. <br /> <br />. A careful analysis, perhaps extending and elaborating <br />the work of Elliott, et al. (1973) should be made of the anticipated <br />effect on streamflow hydrographs and reservoir sto'rage outside the <br />snowpack zone of snow augmentation under a variety of plausible seeding <br />strategies. This shoul~ explic itly include cons ide ration of flood pos s ibilities, <br />which were not dealt with by Elliott, et al. <br /> <br />10 <br />
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