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<br />1353 <br /> <br />before you is a proposal for a two year re- <br />search program to be conducted in three parts. <br />These three parts involve the following acti- <br />vities. <br /> <br />I <br /> <br />In the first part of this proposal, and <br />it is summarized in Mr. Garnsey's first page <br />summary here, the first part of this proposal <br />involves what you might call a study of the <br />kinds of variations that exist in the river <br />flow from historical records, to see how often, <br />for example, from the available actual river <br />flow data, how often, or how probable it is, <br />that a drought, for example, of given dura- <br />tion will occur in the river flow. Now this <br />is looking at past history as simply an exam- <br />ple of what future history is likely to bring. <br />If one looks at this problem from the stand- <br />point of the knowledge that we have of long <br />term trends in weather over the nation at <br />large, one sees that this may not be a safe <br />assumption; but it is the assumption that one <br />must make as the first starting point in going <br />into a program of examination like this. With- <br />out this information one is moving very blindly <br />in trying to forecast what the trend of river <br />flow is likely to be in the specific, say, <br />twenty, thirty, fifty year period ahead of us. <br />So that the first part will be to look at <br />stream flow data to see, for example, how often <br />a drought of one, two, three or four years' <br />duration is likely to occur, using this in- <br />formation, how abundant or how probable it is <br />that there will be from this information, <br />periods of considerable abundance. What is <br />the probability that the river will flow <br />ahead of a given schedule or how probable is <br />it that it will flow behind that given schedule? <br />So that part one deals with specific stream <br />flow data, going into a study of all the <br />scientifically observable information that can <br />be derived from the river flow itself and from <br />using this to precent in the optimum fashion <br />the information as a prediction based on the <br />expectation that the future will be like the <br />past, the prediction of the flow for the river <br />basin. <br /> <br />I <br /> <br />The second part of this study has the ob- <br />jective of looking into the much broader body <br />of weather data that have been taken in the <br />history of Colorado. Weather data of actual <br />precipitation, of temperature, of wind flow, <br />