Počet záznamů: 1  

Comparative validation of statistical and dynamical downscaling models on a dense grid in central Europe: temperature

  1. 1.
    SYSNO ASEP0437127
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevComparative validation of statistical and dynamical downscaling models on a dense grid in central Europe: temperature
    Tvůrce(i) Huth, Radan (UEK-B) RID, ORCID, SAI
    Mikšovský, J. (CZ)
    Štěpánek, Petr (UEK-B) RID, SAI, ORCID
    Belda, M. (CZ)
    Farda, Aleš (UEK-B) RID, SAI
    Chládová, Z. (CZ)
    Pišoft, P. (CZ)
    Zdroj.dok.Theoretical and Applied Climatology - ISSN 0177-798X
    Roč. 120, 3-4 (2015), s. 533-553
    Poč.str.21 s.
    Jazyk dok.eng - angličtina
    Země vyd.AT - Rakousko
    Klíč. slovaatmospheric science ; climatology ; air pollution
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    CEPGAP209/11/2405 GA ČR - Grantová agentura ČR
    ED1.1.00/02.0073 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy
    Institucionální podporaRVO:67179843 - RVO:67179843 ; UFA-U - RVO:68378289
    UT WOS000353220700011
    EID SCOPUS84939892527
    DOI10.1007/s00704-014-1190-3
    AnotaceMinimum and maximum temperature in two regional climate models and five statistical downscaling models are validated according to a unified set of criteria that have a potential relevance for impact assessments: persistence (temporal autocorrelations), spatial autocorrelations, extreme quantiles, skewness, kurtosis, and the degree of fit to observed data on both short and long times scales. The validation is conducted on two dense grids in central Europe as follows: (1) a station network and (2) a grid with a resolution of 10 km. The gridded dataset is not contaminated by artifacts of the interpolation procedure; therefore, we claim that using a gridded dataset as a validation base is a valid approach. The fit to observations in short time scales is equally good for the statistical downscaling (SDS) models and regional climate models (RCMs) in winter, while it is much better for the SDS models in summer. The reproduction of variability on long time scales, expressed as linear trends, is similarly successful by both SDS models and RCMs. Results for other criteria suggest that there is no justification for preferring dynamical models at the expense of statistical models—and vice versa. The non-linear SDS models do not outperform the linear ones.
    PracovištěÚstav výzkumu globální změny
    KontaktNikola Šviková, svikova.n@czechglobe.cz, Tel.: 511 192 268
    Rok sběru2016
Počet záznamů: 1  

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