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    An RCM multi-physics ensemble over Europe: Multi-variable evaluation to avoid error compensation

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    AnRCMMulti-physics.pdf (2.515Mb)
    Identificadores
    URI: http://hdl.handle.net/10902/9842
    DOI: 10.1007/s00382-015-2529-x
    ISSN: 0930-7575
    ISSN: 1432-0894
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    Autoría
    García Díez, MarkelAutoridad Unican; Fernández Fernández, Jesús (matemático)Autoridad Unican; Vautard, Robert
    Fecha
    2015-12
    Derechos
    © Springer. This version of the article has been accepted for publication, after peer review (when applicable) and is subject to Springer Nature's AM terms of use, but is not the Version of Record and does not reflect post-acceptance improvements, or any corrections. The Version of Record is available online at: https://doi.org/10.1007/s00382-015-2529-x
    Publicado en
    Climate Dynamics, 2015, 45(11-12), 3141-3156
    Editorial
    Springer
    Enlace a la publicación
    https://doi.org/10.1007/s00382-015-2529-x
    Palabras clave
    WRF
    CERES
    E-OBS
    GLDAS
    CORDEX
    EURO-CORDEX
    Multi-physics
    Model evaluation
    Radiation
    Soil moisture
    Resumen/Abstract
    Regional Climate Models (RCMs) are widely used tools to add detail to the coarse resolution of global simulations. However, these are known to be affected by biases. Usually, published model evaluations use a reduced number of variables, frequently precipitation and temperature. Due to the complexity of the models, this may not be enough to assess their physical realism (e.g. to enable a fair comparison when weighting ensemble members). Furthermore, looking at only a few variables makes difficult to trace model errors. Thus, in many previous studies, these biases are de- scribed but their underlying causes and mechanisms are often left unknown. In this work the ability of a multi-physics ensemble in reproducing the observed climatologies of any variables over Europe is analysed. These are temperature, precipitation, cloud cover, ra- diative fluxes and total soil moisture content. It is found that, during winter, the model suffers a significant cold bias over snow covered regions. This is shown to be re- lated with a poor representation of the snow-atmosphere interaction, and is amplified by an albedo feedback. It is shown how two members of the ensemble are able to alleviate this bias, but by generating a too large cloud cover. During summer, a large sensitivity to the cumulus parameterization is found, related to large differences in the cloud cover and short wave radiation flux. Results also show that small errors in one variable are sometimes a result of error compensation, so the high dimensionality of the model evaluation problem cannot be disregarded.
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    UNIVERSIDAD DE CANTABRIA

    Repositorio realizado por la Biblioteca Universitaria utilizando DSpace software
    Contacto | Sugerencias
    Metadatos sujetos a:licencia de Creative Commons Reconocimiento 4.0 España