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    Extended Streamflow Forecasting Using NWSRFS

    Source: Journal of Water Resources Planning and Management:;1985:;Volume ( 111 ):;issue: 002
    Author:
    Gerald N. Day
    DOI: 10.1061/(ASCE)0733-9496(1985)111:2(157)
    Publisher: American Society of Civil Engineers
    Abstract: Extended forecasting using the National Weather Service River Forecast System (NWSRFS) is done with the NWS Extended Streamflow Prediction (ESP) program. This paper examines the theory, capabilities, and potential applications of the ESP procedure. ESP uses conceptual hydrologic/hydraulic models to forecast future streamflow using. the current snow, soil moisture, river, and reservoir conditions with historical meteorological data. The ESP procedure assumes that meteorological events that occurred in the past are representative of events that may occur in the future. Each year of historical meteorological data is assumed to be a possible representation of the future and is used to simulate a streamflow trace. The simulated streamflow traces can be scanned for maximum flow, minimum flow, volume of flow, reservoir stage, etc., for any period in the future. ESP produces a probabilistic forecast for each streamflow variable and period of interest. The procedure was originally developed for water supply forecasting in snowmelt areas, but it can also be used to produce spring flood outlooks, forecasts for navigation, inflow hydrographs for reservoir operation, and time series needed for risk analysis during droughts.
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      Extended Streamflow Forecasting Using NWSRFS

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    contributor authorGerald N. Day
    date accessioned2017-05-08T21:06:08Z
    date available2017-05-08T21:06:08Z
    date copyrightApril 1985
    date issued1985
    identifier other%28asce%290733-9496%281985%29111%3A2%28157%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/38726
    description abstractExtended forecasting using the National Weather Service River Forecast System (NWSRFS) is done with the NWS Extended Streamflow Prediction (ESP) program. This paper examines the theory, capabilities, and potential applications of the ESP procedure. ESP uses conceptual hydrologic/hydraulic models to forecast future streamflow using. the current snow, soil moisture, river, and reservoir conditions with historical meteorological data. The ESP procedure assumes that meteorological events that occurred in the past are representative of events that may occur in the future. Each year of historical meteorological data is assumed to be a possible representation of the future and is used to simulate a streamflow trace. The simulated streamflow traces can be scanned for maximum flow, minimum flow, volume of flow, reservoir stage, etc., for any period in the future. ESP produces a probabilistic forecast for each streamflow variable and period of interest. The procedure was originally developed for water supply forecasting in snowmelt areas, but it can also be used to produce spring flood outlooks, forecasts for navigation, inflow hydrographs for reservoir operation, and time series needed for risk analysis during droughts.
    publisherAmerican Society of Civil Engineers
    titleExtended Streamflow Forecasting Using NWSRFS
    typeJournal Paper
    journal volume111
    journal issue2
    journal titleJournal of Water Resources Planning and Management
    identifier doi10.1061/(ASCE)0733-9496(1985)111:2(157)
    treeJournal of Water Resources Planning and Management:;1985:;Volume ( 111 ):;issue: 002
    contenttypeFulltext
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