The 11-year solar cycle in current reanalyses: a (non)linear attribution study of the middle atmosphere
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11320%2F15%3A10317739" target="_blank" >RIV/00216208:11320/15:10317739 - isvavai.cz</a>
Výsledek na webu
<a href="http://dx.doi.org/10.5194/acp-15-6879-2015" target="_blank" >http://dx.doi.org/10.5194/acp-15-6879-2015</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.5194/acp-15-6879-2015" target="_blank" >10.5194/acp-15-6879-2015</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The 11-year solar cycle in current reanalyses: a (non)linear attribution study of the middle atmosphere
Popis výsledku v původním jazyce
This study focusses on the variability of temperature, ozone and circulation characteristics in the stratosphere and lower mesosphere with regard to the influence of the 11-year solar cycle. It is based on attribution analysis using multiple nonlinear techniques (support vector regression, neural networks) besides the multiple linear regression approach. The analysis was applied to several current reanalysis data sets for the 1979-2013 period, including MERRA, ERA-Interim and JRA-55, with the aim to compare how these types of data resolve especially the double-peaked solar response in temperature and ozone variables and the consequent changes induced by these anomalies. Equatorial temperature signals in the tropical stratosphere were found to be in qualitative agreement with previous attribution studies, although the agreement with observational results was incomplete, especially for JRA-55. The analysis also pointed to the solar signal in the ozone data sets (i.e. MERRA and ERA-Interi
Název v anglickém jazyce
The 11-year solar cycle in current reanalyses: a (non)linear attribution study of the middle atmosphere
Popis výsledku anglicky
This study focusses on the variability of temperature, ozone and circulation characteristics in the stratosphere and lower mesosphere with regard to the influence of the 11-year solar cycle. It is based on attribution analysis using multiple nonlinear techniques (support vector regression, neural networks) besides the multiple linear regression approach. The analysis was applied to several current reanalysis data sets for the 1979-2013 period, including MERRA, ERA-Interim and JRA-55, with the aim to compare how these types of data resolve especially the double-peaked solar response in temperature and ozone variables and the consequent changes induced by these anomalies. Equatorial temperature signals in the tropical stratosphere were found to be in qualitative agreement with previous attribution studies, although the agreement with observational results was incomplete, especially for JRA-55. The analysis also pointed to the solar signal in the ozone data sets (i.e. MERRA and ERA-Interi
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
—
Návaznosti výsledku
Projekt
—
Návaznosti
S - Specificky vyzkum na vysokych skolach<br>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
Atmospheric Chemistry and Physics
ISSN
1680-7316
e-ISSN
—
Svazek periodika
15
Číslo periodika v rámci svazku
12
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
17
Strana od-do
6879-6895
Kód UT WoS článku
000357117500022
EID výsledku v databázi Scopus
2-s2.0-84934991404