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<br />, <br /> <br />~ <br /> <br />003356 <br /> <br />The analyses involve the establishing of historical relations for <br /> <br /> <br />both precipitation and streamflow with physical model calculations of basin <br /> <br /> <br />wide precipitation. The numerical model calculations input atmospheric <br /> <br /> <br />parameters that control the orographic cloud processes. Hhile it has <br /> <br />been shown that this approach provides a useful assessment approach it is <br /> <br /> <br />unlikely (but not impossible) that differences from expectency would <br /> <br /> <br />be statistically significant for only one operational year. The data <br /> <br /> <br />from last year's limited program and from any subsequent application <br /> <br /> <br />programs in the state can be used directly in this type of analysis <br /> <br />to provide an increasingly improved estimate of seeding effects. <br /> <br />11 <br />