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    Evaluation of Two Land Surface Schemes Used in Terrains of Increasing Aridity in West Africa

    Source: Journal of Hydrometeorology:;2008:;Volume( 009 ):;issue: 002::page 173
    Author:
    Schüttemeyer, D.
    ,
    Moene, A. F.
    ,
    Holtslag, A. A. M.
    ,
    de Bruin, H. A. R.
    DOI: 10.1175/2007JHM797.1
    Publisher: American Meteorological Society
    Abstract: In this study different parameterizations for land surface models currently employed in meteorological models at ECMWF [Tiled ECMWF Surface Scheme for Exchange Processes over Land (TESSEL)] and NCEP (Noah) are evaluated for a semiarid region in Ghana, West Africa. Both schemes utilize the Jarvis?Stewart approach to calculate canopy conductance as the critical variable for partitioning the available energy into sensible and latent heat flux. Additionally, an approach within Noah is tested to calculate canopy conductance based on plant physiology (A-gs method), where the photosynthetic assimilation is coupled to the leaf stomatal conductance. All parameterizations were run offline for a seasonal cycle in 2002/03 using observations as forcings at two test sites. The two locations are in the humid tropical southern region and in the drier northern region. For the purpose of forcing and evaluation, a new set of data has been utilized to include surface fluxes obtained by scintillometry. The measurements include the rapid wet-to-dry transition after the wet season at both sites. As a general trend, it has been found that during the wet period of a season net radiation is described well by all parameterizations. During the drying process the errors in modeled net radiation increased at both sites. The models perform poorly in simulating soil heat fluxes with larger errors for TESSEL for both sites. The evolution in time for sensible heat flux and latent heat flux was tackled in different ways by the utilized parameterizations and sites with enhanced model performance for the more southern site. Soil moisture in the upper soil layers is modeled with small errors for the different parameterizations. Key adjustments for reducing net radiation during the dry period of a season are discussed. In particular, the ratio of roughness length of momentum and heat was found to be an important parameter, but will require seasonal adjustments.
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      Evaluation of Two Land Surface Schemes Used in Terrains of Increasing Aridity in West Africa

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4207174
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    contributor authorSchüttemeyer, D.
    contributor authorMoene, A. F.
    contributor authorHoltslag, A. A. M.
    contributor authorde Bruin, H. A. R.
    date accessioned2017-06-09T16:19:55Z
    date available2017-06-09T16:19:55Z
    date copyright2008/04/01
    date issued2008
    identifier issn1525-755X
    identifier otherams-65899.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4207174
    description abstractIn this study different parameterizations for land surface models currently employed in meteorological models at ECMWF [Tiled ECMWF Surface Scheme for Exchange Processes over Land (TESSEL)] and NCEP (Noah) are evaluated for a semiarid region in Ghana, West Africa. Both schemes utilize the Jarvis?Stewart approach to calculate canopy conductance as the critical variable for partitioning the available energy into sensible and latent heat flux. Additionally, an approach within Noah is tested to calculate canopy conductance based on plant physiology (A-gs method), where the photosynthetic assimilation is coupled to the leaf stomatal conductance. All parameterizations were run offline for a seasonal cycle in 2002/03 using observations as forcings at two test sites. The two locations are in the humid tropical southern region and in the drier northern region. For the purpose of forcing and evaluation, a new set of data has been utilized to include surface fluxes obtained by scintillometry. The measurements include the rapid wet-to-dry transition after the wet season at both sites. As a general trend, it has been found that during the wet period of a season net radiation is described well by all parameterizations. During the drying process the errors in modeled net radiation increased at both sites. The models perform poorly in simulating soil heat fluxes with larger errors for TESSEL for both sites. The evolution in time for sensible heat flux and latent heat flux was tackled in different ways by the utilized parameterizations and sites with enhanced model performance for the more southern site. Soil moisture in the upper soil layers is modeled with small errors for the different parameterizations. Key adjustments for reducing net radiation during the dry period of a season are discussed. In particular, the ratio of roughness length of momentum and heat was found to be an important parameter, but will require seasonal adjustments.
    publisherAmerican Meteorological Society
    titleEvaluation of Two Land Surface Schemes Used in Terrains of Increasing Aridity in West Africa
    typeJournal Paper
    journal volume9
    journal issue2
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/2007JHM797.1
    journal fristpage173
    journal lastpage193
    treeJournal of Hydrometeorology:;2008:;Volume( 009 ):;issue: 002
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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