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    Parameterization of the Urban Water Budget with the Submesoscale Soil Model

    Source: Journal of Applied Meteorology and Climatology:;2006:;volume( 045 ):;issue: 004::page 624
    Author:
    Dupont, Sylvain
    ,
    Mestayer, Patrice G.
    ,
    Guilloteau, Emmanuel
    ,
    Berthier, Emmanuel
    ,
    Andrieu, Hervé
    DOI: 10.1175/JAM2363.1
    Publisher: American Meteorological Society
    Abstract: This paper presents the hydrological component of the Submesoscale Soil Model, urbanized version (SM2-U). This model is an extension of the rural Interactions between Soil, Biosphere, and Atmosphere (ISBA) soil model to urban surfaces. It considers in detail both rural and urban surfaces. Its purpose is to compute the sensible heat and humidity fluxes at the canopy?atmosphere interface for the computational domain lower boundary condition of atmospheric mesoscale models in order to simulate the urban boundary layer in any weather conditions. Because it computes separately the surface temperature of each land use cover mode while the original model computes a unique temperature for the soil and vegetation system, the new version is first validated for rural grounds by comparison with experimental data from the Hydrological Atmospheric Pilot Experiment-Modélisation du Bilan Hydrique (HAPEX-MOBILHY) and the European Field Experiment in a Desertification Threatened Area (EFEDA). The SM2-U water budget is then evaluated on the experimental data obtained at a suburban site in the Nantes urban area (Rezé, France), both on an annual scale and for two stormy events. SM2-U evaluates correctly the water flow measured in the drainage network (DN) at the annual scale and for the summer storm. As for the winter storm, when the soil is saturated, the simulation shows that water infiltration from the soil to the DN must be taken care of to evaluate correctly the DN flow. Yet, the addition of this soil water infiltration to the DN does not make any difference in the simulated surface fluxes that are the model outputs for simulating the urban boundary layer. Urban hydrological parameters are shown to largely influence the available water on artificial surfaces for evaporation and to influence less the evapotranspiration from natural surfaces. The influence of the water budget and surface structure on the suburban site local climatology is demonstrated.
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      Parameterization of the Urban Water Budget with the Submesoscale Soil Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4216505
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    • Journal of Applied Meteorology and Climatology

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    contributor authorDupont, Sylvain
    contributor authorMestayer, Patrice G.
    contributor authorGuilloteau, Emmanuel
    contributor authorBerthier, Emmanuel
    contributor authorAndrieu, Hervé
    date accessioned2017-06-09T16:47:52Z
    date available2017-06-09T16:47:52Z
    date copyright2006/04/01
    date issued2006
    identifier issn1558-8424
    identifier otherams-74296.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4216505
    description abstractThis paper presents the hydrological component of the Submesoscale Soil Model, urbanized version (SM2-U). This model is an extension of the rural Interactions between Soil, Biosphere, and Atmosphere (ISBA) soil model to urban surfaces. It considers in detail both rural and urban surfaces. Its purpose is to compute the sensible heat and humidity fluxes at the canopy?atmosphere interface for the computational domain lower boundary condition of atmospheric mesoscale models in order to simulate the urban boundary layer in any weather conditions. Because it computes separately the surface temperature of each land use cover mode while the original model computes a unique temperature for the soil and vegetation system, the new version is first validated for rural grounds by comparison with experimental data from the Hydrological Atmospheric Pilot Experiment-Modélisation du Bilan Hydrique (HAPEX-MOBILHY) and the European Field Experiment in a Desertification Threatened Area (EFEDA). The SM2-U water budget is then evaluated on the experimental data obtained at a suburban site in the Nantes urban area (Rezé, France), both on an annual scale and for two stormy events. SM2-U evaluates correctly the water flow measured in the drainage network (DN) at the annual scale and for the summer storm. As for the winter storm, when the soil is saturated, the simulation shows that water infiltration from the soil to the DN must be taken care of to evaluate correctly the DN flow. Yet, the addition of this soil water infiltration to the DN does not make any difference in the simulated surface fluxes that are the model outputs for simulating the urban boundary layer. Urban hydrological parameters are shown to largely influence the available water on artificial surfaces for evaporation and to influence less the evapotranspiration from natural surfaces. The influence of the water budget and surface structure on the suburban site local climatology is demonstrated.
    publisherAmerican Meteorological Society
    titleParameterization of the Urban Water Budget with the Submesoscale Soil Model
    typeJournal Paper
    journal volume45
    journal issue4
    journal titleJournal of Applied Meteorology and Climatology
    identifier doi10.1175/JAM2363.1
    journal fristpage624
    journal lastpage648
    treeJournal of Applied Meteorology and Climatology:;2006:;volume( 045 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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