Climate impacts of the NAO are sensitive to how the NAO is defined
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10297872" target="_blank" >RIV/00216208:11310/15:10297872 - isvavai.cz</a>
Nalezeny alternativní kódy
RIV/67179843:_____/15:00432100 RIV/68378289:_____/15:00432100
Výsledek na webu
<a href="http://dx.doi.org/10.1007/s00704-014-1116-0" target="_blank" >http://dx.doi.org/10.1007/s00704-014-1116-0</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s00704-014-1116-0" target="_blank" >10.1007/s00704-014-1116-0</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Climate impacts of the NAO are sensitive to how the NAO is defined
Popis výsledku v původním jazyce
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 sensitivit
Název v anglickém jazyce
Climate impacts of the NAO are sensitive to how the NAO is defined
Popis výsledku anglicky
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 sensitivit
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DG - Vědy o atmosféře, meteorologie
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2015
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Theorectical and Applied Climatology
ISSN
0177-798X
e-ISSN
—
Svazek periodika
119
Číslo periodika v rámci svazku
3-4
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
14
Strana od-do
639-652
Kód UT WoS článku
000349020900017
EID výsledku v databázi Scopus
2-s2.0-84948614435