PPT-1 Recent Improvements to the GOES-R Rainfall Rate Algorithm

Author : calandra-battersby | Published Date : 2016-07-17

1 July 2015 Presented By Bob Kuligowski NOAANESDISSTAR Yaping Li Yan Hao I M Systems Group 2 Outline Background Motivation Satellite QPE Basics The Basic GOESR

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1 Recent Improvements to the GOES-R Rainfall Rate Algorithm: Transcript


1 July 2015 Presented By Bob Kuligowski NOAANESDISSTAR Yaping Li Yan Hao I M Systems Group 2 Outline Background Motivation Satellite QPE Basics The Basic GOESR Rainfall Rate Algorithm. L.R. . Rabiner. and M.R. . Sambur. The Bell System Technical Journal. , Vol. 54, No. 2, Feb. 1975, pp. 297-315. Outline. Intro to problem. Solution. Algorithm. Summary. Motivation. Word recognition needs to detect word boundaries in speech. Michael L. Jurewicz, Sr.. WFO Binghamton, NY. Northeast Regional Operational Workshop. November 5, 2009 . AR TC Tracks and PRE Locations. All AR TC Tracks. . All AR PPTC Tracks; with PRE centroids (colored dots). flow. (Mays p 310-321). Learning objective. Be able to calculate infiltration, cumulative infiltration and time to ponding using the Green-. Ampt. method as given in Mays Section . 7.4. The rate at which water can infiltrate is important for determining the partition between whether rainfall infiltrates or becomes runoff that flows overland to streams.. Critical Design Review. September 9, 2011. Prepared By:. Limin Zhao. 2. , Bob Kuligowski. 1. , Clay Davenport. 3. , and Walter Wolf. 1. 1. NOAA/NESDIS/STAR. 2. NOAA/NESDIS/OSPO. 3. SSAI. 2. Review Agenda. Absorption, scattering and extinction cross sections.. Backscattering cross section.. Cross section in the Rayleigh limit (particle diameter is much smaller than the wavelength of the radiation.). Radar cross section for a particle in the Rayleigh limit.. Critical Design Review. September 9, 2011. Prepared By:. Limin Zhao. 2. , Bob Kuligowski. 1. , Clay Davenport. 3. , and Walter Wolf. 1. 1. NOAA/NESDIS/STAR. 2. NOAA/NESDIS/OSPO. 3. SSAI. 2. Review Agenda. Absorption, scattering and extinction cross sections.. Backscattering cross section.. Cross section in the Rayleigh limit (particle diameter is much smaller than the wavelength of the radiation.). Radar cross section for a particle in the Rayleigh limit.. Radar: The Quickest Path to dbZ Absorption, scattering and extinction cross sections. Backscattering cross section. Cross section in the Rayleigh limit (particle diameter is much smaller than the wavelength of the radiation.) Include Week-1 and Week-2 Outlooks . Update prepared by. Climate Prediction Center / NCEP. 29 July . 2019. For more information, visit:. http://www.cpc.ncep.noaa.gov/products/Global_Monsoons/African_Monsoons/precip_monitoring.shtml. Include Week-1 and Week-2 Outlooks . Update prepared by. Climate Prediction Center / NCEP. 02 December 2019. For more information, visit:. http://www.cpc.ncep.noaa.gov/products/Global_Monsoons/African_Monsoons/precip_monitoring.shtml. Include Week-1 and Week-2 Outlooks . Update prepared by. Climate Prediction Center / NCEP. 24 August 2020. For more information, visit:. http://www.cpc.ncep.noaa.gov/products/Global_Monsoons/African_Monsoons/precip_monitoring.shtml. Usman Mohseni1, Sai Bargav Muskula2. 1,2Research Scholar, Department of Civil Engineering, IIT Roorkee, Roorkee, INDIA. INTRODUCTION. Rainfall-runoff modelling is one of the most prominent hydrological models used to examine the relation between rainfall and runoff . Water entering the soil at the ground surface . It replenishes the soil moisture deficiency and the excess moves downward by force of gravity called deep seepage or percolation and builds up the ground water table . From Mays, 2011, Ground and Surface Water Hydrology. A D hour unit hydrograph is the characteristic response of a given watershed to a unit volume (e.g. 1 in or cm) of effective water input (usually rain) applied at a constant rate for D hours.

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