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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />..: <br /> <br />, <br /> <br />4.0 Conclusion <br /> <br />In conclusion a simple but useful SkewT -LogP based quantitative convective <br />precipitation potential (QCP2) technique was described as an aid in flash flood <br />prediction. The technique related the depth of the updraft that is warmer than OC or the <br />updraft warm layer (UWL) to the precipitation efficiency and potential of the <br />thunderstorm based on the formation of warm coalescence rain mechanisms. The peak <br />60 minute rainfall potential was related by an equation to the surface to 500mb <br />precipitable water index and a regional warm layer value. <br /> <br />In general the QCP2 notes the enhanced ability of thunderstorm updrafts to process <br />more than twice the estimated PWI in a one hour period when the warm layer of the <br />updraft equals or exceeds 1.5 kIn a t elevations above 3,500 feet, 2.5 kIn at elevations <br />below 3,500 feet and 3.5 kIn when the surface dew points exceed 70F. <br /> <br />The QCP2 calculation technique could be adapted for use in the NWS SHARP <br />program and initialized hourly on ASOS or local mesonet observations. In data rich <br />observation areas such as the Oklahoma Mesonet statewide QCP2 could be easily <br />obtained for use in the issuance of flash flood predictions and for use by River Forecast <br />Center products based on QPF. The author has had some additional success in using <br />the QCP2 to "atmosphere-truth" the Z-R relationship in the WSR-88D to assist in <br />the preparation of radar-precipitation mapping products. <br /> <br />The QCP2 technique has been used successfully by the author over the past 14 years in <br />the Denver F2P2 on an almost daily basis for the issuance of a variety of heavy <br />precipitation products in support of the Denver emergency response community, The <br />technique requires the user to possess both predictive and analytic skills which can <br />be applied in a stressful operational environment. Yet it is simple enough to easily <br />be assimilated into most forecast routines and provide reliable assistance to crucial <br />decision-making during flash flooding situations. <br /> <br />Clearly the thunderstorm and flash flooding QPF is one of the most vexing forecast <br />problems facing the operational meteorologist. It is hoped that the QCP2 technique will <br />prove to be"a reliable asset during flash flood forecast situations to the forecaster until <br />more sophisticated techniques and tools can be provided by the research and operational <br />communities. <br /> <br />Acknowledgements: The author apologizes for the late submittal of this manwcript Effective time useage is a <br />problem he is addressing. Special thanks are due to Dennis Sims of the old GRD Weather Center, Ron Kelly of the <br />old Henz Kelly & Associates and Bryan Rappolt and Frank RobItaille of Henz Meteorological Services for the <br />effective contributions they made in assisting the author in the refmement of the QCP2 technique and the effective <br />operational application of QCP2 in the Denver P2P2 for the past 14 yean;. <br /> <br />References <br /> <br />Henz. J.F., 1993: Operationally Predictable Updraft Characteristics of Heavy Precipitation Producing Thunderstorms, 847.849. <br />Preprints of the 16th Conference on Severe Local Stonos, October 1993. St.Louis. Missouri. American Meteorological Society. <br /> <br />5 <br />