Počet záznamů: 1  

Climate impacts of the NAO are sensitive to how the NAO is defined

  1. 1.
    SYSNO ASEP0432100
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevClimate impacts of the NAO are sensitive to how the NAO is defined
    Tvůrce(i) Pokorná, Lucie (UFA-U) RID, ORCID
    Huth, Radan (UEK-B) RID, ORCID, SAI
    Zdroj.dok.Theoretical and Applied Climatology - ISSN 0177-798X
    Roč. 119, 3-4 (2015), s. 639-652
    Poč.str.14 s.
    Forma vydáníTištěná - P
    Jazyk dok.eng - angličtina
    Země vyd.AT - Rakousko
    Klíč. slovaNorth-Atlantic-Oscillation ; atmospheric circulation ; winter temperature ; variability modes ; time variations ; Icelandic low ; precipitation ; surface ; frequency ; Europe
    Vědní obor RIVDG - Vědy o atmosféře, meteorologie
    CEPGAP209/10/2265 GA ČR - Grantová agentura ČR
    ED1.1.00/02.0073 GA MŠMT - Ministerstvo školství, mládeže a tělovýchovy
    Institucionální podporaUFA-U - RVO:68378289 ; RVO:67179843 - RVO:67179843
    UT WOS000349020900017
    EID SCOPUS84948614435
    DOI10.1007/s00704-014-1116-0
    AnotaceWe analyze the sensitivity of the effects the North Atlantic Oscillation (NAO) exerts on surface temperature and precipitation in Europe to the definition of the NAO index. Seven different NAO indices are examined: two based on station sea level pressure (SLP) data, two based on action centers, and three based on correlation/covariance structures described by principal component analysis (PCA). The analysis is based on monthly mean data; winter and summer seasons are analyzed separately. Temporal correlations between indices are weaker in summer than in winter for most pairs of indices. In particular, low correlations are found between station indices on the one hand and PCA-based indices on the other hand. The NAO effects are quantified by correlations between the indices and station data in Europe. Effects of the NAO on precipitation amount and wet day probability are very similar, while NAO effects on maximum temperature are stronger than those on minimum temperature. The sensitivity of the NAO effects on both surface temperature and precipitation to the choice of the NAO index is considerably higher in summer. Correlations differ among the NAO indices not only in their magnitude but in some regions in summer also in their sign.
    PracovištěÚstav fyziky atmosféry
    KontaktKateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019
    Rok sběru2016
Počet záznamů: 1  

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