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    The Influence of Hydrologic Modeling on the Predicted Local Weather: Two-Way Coupling of a Mesoscale Weather Prediction Model and a Land Surface Hydrologic Model

    Source: Journal of Hydrometeorology:;2002:;Volume( 003 ):;issue: 005::page 505
    Author:
    Seuffert, G.
    ,
    Gross, P.
    ,
    Simmer, C.
    ,
    Wood, E. F.
    DOI: 10.1175/1525-7541(2002)003<0505:TIOHMO>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: A two-way coupling of the operational mesoscale weather prediction model known as Lokal Modell (LM; German Weather Service) with the land surface hydrologic ?TOPMODEL?-Based Land Surface?Atmosphere Transfer Scheme (TOPLATS; Princeton University) has been carried out to investigate the influence of a ?state-of-the-art? land surface hydrologic model on the predicted local weather. Two case studies are presented that quantify the influence of the combined modeling system on the turbulent fluxes and boundary layer structure and on the formation of precipitation. The model results are compared with ground-based measurements of turbulent fluxes, boundary layer structure, and precipitation. Furthermore, whether the initialization of the original LM with more realistic soil moisture fields would be sufficient to improve the weather forecast is investigated. The results of the two case studies show that, when compared with measurements, the two-way coupled modeling system using TOPLATS improves the predicted energy fluxes and rain amount in comparison with predictions from the original LM. The initialization of the LM just using soil moisture fields based on TOPLATS does not result in an improvement of the local weather forecast: although the simulation of the sensible and latent heat fluxes is improved, the representation of the boundary layer structure is not captured well. In the original LM, the surface processes are not modeled in sufficient detail, which resulted in significant overprediction of precipitation for one case study. The main reason for the improved performance of the two-way coupled modeling system on the basis of TOPLATS probably is the more accurate representation of vegetation and soil hydrologic processes. This results in more realistically simulated soil moisture fields and better simulation of the dynamic range of the surface temperature when compared with the other model configurations.
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      The Influence of Hydrologic Modeling on the Predicted Local Weather: Two-Way Coupling of a Mesoscale Weather Prediction Model and a Land Surface Hydrologic Model

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4206231
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    contributor authorSeuffert, G.
    contributor authorGross, P.
    contributor authorSimmer, C.
    contributor authorWood, E. F.
    date accessioned2017-06-09T16:17:16Z
    date available2017-06-09T16:17:16Z
    date copyright2002/10/01
    date issued2002
    identifier issn1525-755X
    identifier otherams-65049.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4206231
    description abstractA two-way coupling of the operational mesoscale weather prediction model known as Lokal Modell (LM; German Weather Service) with the land surface hydrologic ?TOPMODEL?-Based Land Surface?Atmosphere Transfer Scheme (TOPLATS; Princeton University) has been carried out to investigate the influence of a ?state-of-the-art? land surface hydrologic model on the predicted local weather. Two case studies are presented that quantify the influence of the combined modeling system on the turbulent fluxes and boundary layer structure and on the formation of precipitation. The model results are compared with ground-based measurements of turbulent fluxes, boundary layer structure, and precipitation. Furthermore, whether the initialization of the original LM with more realistic soil moisture fields would be sufficient to improve the weather forecast is investigated. The results of the two case studies show that, when compared with measurements, the two-way coupled modeling system using TOPLATS improves the predicted energy fluxes and rain amount in comparison with predictions from the original LM. The initialization of the LM just using soil moisture fields based on TOPLATS does not result in an improvement of the local weather forecast: although the simulation of the sensible and latent heat fluxes is improved, the representation of the boundary layer structure is not captured well. In the original LM, the surface processes are not modeled in sufficient detail, which resulted in significant overprediction of precipitation for one case study. The main reason for the improved performance of the two-way coupled modeling system on the basis of TOPLATS probably is the more accurate representation of vegetation and soil hydrologic processes. This results in more realistically simulated soil moisture fields and better simulation of the dynamic range of the surface temperature when compared with the other model configurations.
    publisherAmerican Meteorological Society
    titleThe Influence of Hydrologic Modeling on the Predicted Local Weather: Two-Way Coupling of a Mesoscale Weather Prediction Model and a Land Surface Hydrologic Model
    typeJournal Paper
    journal volume3
    journal issue5
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/1525-7541(2002)003<0505:TIOHMO>2.0.CO;2
    journal fristpage505
    journal lastpage523
    treeJournal of Hydrometeorology:;2002:;Volume( 003 ):;issue: 005
    contenttypeFulltext
    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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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian