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<br />cyclical storage could be drawn in greater amounts without <br />risking shortages to meet prior commitments. Storage water <br />held in abeyance as governed under critical water conditions <br />could be released ahead and the;reby fully utilized, instead of <br />being wasted. Based on advance knowledge of resources, <br />industry could schedule production and avoid abrupt curtail- <br />ments 0 <br /> <br />Flood Control - Water spilled to provide flood control could <br />be conserved to generate power or to meet other conservation <br />uses later. Flood plains could be profitably farmed and <br />harvested during periods of forecasted low runoff. Pro- <br />tective measures could be taken much time ahead during <br />periods of forecasted high floods. <br /> <br />Irrigation - Prior knowledge on runoff would modify the <br />irrigated and non-irrigated cropping practice. Releases <br />could be made to supplement water supply to lands now <br />inadequately irrigated. Stored for irrigation, water could <br />safely be released in advance when needed to provide addi- <br />tional flood control space. <br /> <br />Streamflow forecasting procedures described herein are an adap- <br />tation of the methods of ultra long range weather forecasting, evolved during <br />the last 25 years by the staff of the American Institute of Aerological Re- <br />search. The work began at the California Institute of Technology where the <br />author and his associates directed the activities of the Department of Mete- <br />orology between 1933 and 1948. <br /> <br />The method involves the discovery and analysis of systematic <br />behavior features of globe-circling atmO'spheric pressure waves. The con- <br />clusions reached are derived from an examination of historical weather data <br />in the form of Northern Hemispheric daily surface weather charts on which <br />the barometric pressure patterns are drawn. It has been found possible to <br />classify into various categories sequential pressure patterns, representing <br />fundamentally stable flow patterns in the atmosphere. These patterns are <br />called weather types. <br /> <br />The reality of such a classification confirms the ordered nature of <br />atmospheric behavior and the fact that the wind systems have certain preferred <br />positions in relation to the !!;eographic features of the earth's surface, and the <br />terrestrial and extra-terrestrial forces pulsing the atmosphere. The catalog <br />of weather types, prepared from an examination of the historical archive of <br />Northern Hemispheric daily weather cha;rts, becomes a useful tool in fore- <br />casting because it provides a meanS of n:>aking full use of historical data in <br /> <br />- 16 - <br /> <br />