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

0432100 - ÚFA 2016 RIV AT eng J - Článek v odborném periodiku
Pokorná, Lucie - Huth, Radan
Climate impacts of the NAO are sensitive to how the NAO is defined.
Theoretical and Applied Climatology. Roč. 119, 3-4 (2015), s. 639-652. ISSN 0177-798X. E-ISSN 1434-4483
Grant CEP: GA ČR GAP209/10/2265; GA MŠMT(CZ) ED1.1.00/02.0073
Institucionální podpora: RVO:68378289 ; RVO:67179843
Klíčová slova: North-Atlantic-Oscillation * atmospheric circulation * winter temperature * variability modes * time variations * Icelandic low * precipitation * surface * frequency * Europe
Kód oboru RIV: DG - Vědy o atmosféře, meteorologie
Impakt faktor: 2.433, rok: 2015
http://link.springer.com/article/10.1007%2Fs00704-014-1116-0

We 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.
Trvalý link: http://hdl.handle.net/11104/0236634