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<br />cil has adopted the Log-Pearson Type III distribution <br />for use in statistically analyzing !;treamflow data at a <br />single location. A good rE!ference covering the details <br />of the computation procedure when applying the Log <br />Pearson Type III Distribution to the analysis of <br />streamflow data is available from the U.S. Water Re- <br />sources Council (See Reference No. :!). <br /> <br />References <br /> <br />1) Water Resources Publications, Frequency <br />and Risk Analysis in Hydrology, G.W. Kite, <br />1977 . <br /> <br />2)U.S. Water Resources Council, Guidelines <br />for Determini.ng Flood Flow Frequency (Bulle- <br />tin 17), 2120 L street N.W., Washington D.C. <br />20037, June, 1977. <br /> <br />MultiplE! Location statistioal AnalY!lis <br /> <br />Multiple Location Statistical Analysis involves the <br />statistical Analysis of Recorded Hydrologic Data for <br />use in ::1aking statistical Infenmce at other Locations. <br />This procedure has been used in the development of <br />isohyetal maps for rainfall atlases. The National <br />Oceanic and Atmospheric Administration (NOAA) has <br />completed a comprehensive analysis of all Weather <br />Bureau ,Stations throughout the united States that allow <br />for relatively accuratE!: prediction of rainfall amounts <br />for various return periods and durations. The rainfall <br />amount for a given return. period and duration is ob- <br />tai.ned i:JY interpolation between isohyetals or "rainfall <br />contours." The most widely used Rainfall Atlas for <br />many years was Technical :?aper 40 by the U. S. Weather <br />Bureau. More recently, Technical Paper 40 has been <br />supplan':ed by the NOAA Western l\tlas (See Ref,erence No. <br />3) . <br /> <br />!:~ <br />