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    Diffusion Wave Modeling of Distributed Catchment Dynamics

    Source: Journal of Hydrologic Engineering:;1996:;Volume ( 001 ):;issue: 003
    Author:
    Stefano Orlandini
    ,
    Renzo Rosso
    DOI: 10.1061/(ASCE)1084-0699(1996)1:3(103)
    Publisher: American Society of Civil Engineers
    Abstract: A diffusion wave model of distributed catchment dynamics is presented. The effects of catchment topography and river network structure on storm-flow response are incorporated by routing surface runoff in cascade throughout a digital elevation model (DEM) based conceptual transport network, where the Muskingum-Cunge scheme with variable parameters is used to describe surface runoff dynamics. Dynamic scaling of hydraulic geometry is also incorporated in the model by using the “at-a-station” and “downstream” relationships by Leopold and Maddock. Numerical experiments indicate that the model is more than 98% mass conservative for possible slope and roughness configurations, which may occur for hillslopes in a natural catchment. Fluctuations in the simulated discharge may occur in response to discontinuities in rainfall excess representation if Courant number
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      Diffusion Wave Modeling of Distributed Catchment Dynamics

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    http://yetl.yabesh.ir/yetl1/handle/yetl/49347
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    contributor authorStefano Orlandini
    contributor authorRenzo Rosso
    date accessioned2017-05-08T21:23:04Z
    date available2017-05-08T21:23:04Z
    date copyrightJuly 1996
    date issued1996
    identifier other%28asce%291084-0699%281996%291%3A3%28103%29.pdf
    identifier urihttp://yetl.yabesh.ir/yetl/handle/yetl/49347
    description abstractA diffusion wave model of distributed catchment dynamics is presented. The effects of catchment topography and river network structure on storm-flow response are incorporated by routing surface runoff in cascade throughout a digital elevation model (DEM) based conceptual transport network, where the Muskingum-Cunge scheme with variable parameters is used to describe surface runoff dynamics. Dynamic scaling of hydraulic geometry is also incorporated in the model by using the “at-a-station” and “downstream” relationships by Leopold and Maddock. Numerical experiments indicate that the model is more than 98% mass conservative for possible slope and roughness configurations, which may occur for hillslopes in a natural catchment. Fluctuations in the simulated discharge may occur in response to discontinuities in rainfall excess representation if Courant number
    publisherAmerican Society of Civil Engineers
    titleDiffusion Wave Modeling of Distributed Catchment Dynamics
    typeJournal Paper
    journal volume1
    journal issue3
    journal titleJournal of Hydrologic Engineering
    identifier doi10.1061/(ASCE)1084-0699(1996)1:3(103)
    treeJournal of Hydrologic Engineering:;1996:;Volume ( 001 ):;issue: 003
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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