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    New Estimates of Variations in Water Flux and Storage over Europe Based on Regional (Re)Analyses and Multisensor Observations

    Source: Journal of Hydrometeorology:;2014:;Volume( 015 ):;issue: 006::page 2397
    Author:
    Springer, Anne
    ,
    Kusche, Jürgen
    ,
    Hartung, Kerstin
    ,
    Ohlwein, Christan
    ,
    Longuevergne, Laurent
    DOI: 10.1175/JHM-D-14-0050.1
    Publisher: American Meteorological Society
    Abstract: recipitation minus evapotranspiration, the net flux of water between the atmosphere and Earth?s surface, links atmospheric and terrestrial water budgets and thus represents an important boundary condition for both climate modeling and hydrological studies. However, the atmospheric?terrestrial flux is poorly constrained by direct observations because of a lack of unbiased measurements. Thus, it is usually reconstructed from atmospheric reanalyses. Via the terrestrial water budget equation, water storage estimates from the Gravity Recovery and Climate Experiment (GRACE) combined with measured river discharge can be used to assess the realism of the atmospheric?terrestrial flux in models. In this contribution, the closure of the terrestrial water budget is assessed over a number of European river basins using the recently reprocessed GRACE release 05 data, together with precipitation and evapotranspiration from the operational analyses of high-resolution, limited-area NWP models [Consortium for Small-Scale Modelling, German version (COSMO-DE) and European version (COSMO-EU)] and the new COSMO 6-km reanalysis (COSMO-REA6) for the European Coordinated Regional Climate Downscaling Experiment (CORDEX) domain. These closures are compared to those obtained with global reanalyses, land surface models, and observation-based datasets. The spatial resolution achieved with the recent GRACE data allows for better evaluation of the water budget in smaller river basins than before and for the identification of biases up to 25 mm month?1 in the different products. Variations of deseasoned and detrended atmospheric?terrestrial flux are found to agree notably well with flux derived from GRACE and discharge data with correlations up to 0.75. Finally, bias-corrected fluxes are derived from various data combinations, and from this, a 20-yr time series of catchment-integrated water storage variations is reconstructed.
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      New Estimates of Variations in Water Flux and Storage over Europe Based on Regional (Re)Analyses and Multisensor Observations

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    contributor authorSpringer, Anne
    contributor authorKusche, Jürgen
    contributor authorHartung, Kerstin
    contributor authorOhlwein, Christan
    contributor authorLonguevergne, Laurent
    date accessioned2017-06-09T17:15:55Z
    date available2017-06-09T17:15:55Z
    date copyright2014/12/01
    date issued2014
    identifier issn1525-755X
    identifier otherams-82081.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4225155
    description abstractrecipitation minus evapotranspiration, the net flux of water between the atmosphere and Earth?s surface, links atmospheric and terrestrial water budgets and thus represents an important boundary condition for both climate modeling and hydrological studies. However, the atmospheric?terrestrial flux is poorly constrained by direct observations because of a lack of unbiased measurements. Thus, it is usually reconstructed from atmospheric reanalyses. Via the terrestrial water budget equation, water storage estimates from the Gravity Recovery and Climate Experiment (GRACE) combined with measured river discharge can be used to assess the realism of the atmospheric?terrestrial flux in models. In this contribution, the closure of the terrestrial water budget is assessed over a number of European river basins using the recently reprocessed GRACE release 05 data, together with precipitation and evapotranspiration from the operational analyses of high-resolution, limited-area NWP models [Consortium for Small-Scale Modelling, German version (COSMO-DE) and European version (COSMO-EU)] and the new COSMO 6-km reanalysis (COSMO-REA6) for the European Coordinated Regional Climate Downscaling Experiment (CORDEX) domain. These closures are compared to those obtained with global reanalyses, land surface models, and observation-based datasets. The spatial resolution achieved with the recent GRACE data allows for better evaluation of the water budget in smaller river basins than before and for the identification of biases up to 25 mm month?1 in the different products. Variations of deseasoned and detrended atmospheric?terrestrial flux are found to agree notably well with flux derived from GRACE and discharge data with correlations up to 0.75. Finally, bias-corrected fluxes are derived from various data combinations, and from this, a 20-yr time series of catchment-integrated water storage variations is reconstructed.
    publisherAmerican Meteorological Society
    titleNew Estimates of Variations in Water Flux and Storage over Europe Based on Regional (Re)Analyses and Multisensor Observations
    typeJournal Paper
    journal volume15
    journal issue6
    journal titleJournal of Hydrometeorology
    identifier doi10.1175/JHM-D-14-0050.1
    journal fristpage2397
    journal lastpage2417
    treeJournal of Hydrometeorology:;2014:;Volume( 015 ):;issue: 006
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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