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Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008
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SYSNO ASEP 0367983 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Long term variability of total ozone yearly minima and maxima in the latitudinal belt from 20° N to 60° N derived from the merged satellite data in the period 1979-2008 Author(s) Križan, Peter (UFA-U) RID, ORCID
Mikšovský, J. (CZ)
Kozubek, Michal (CZ)
Wang, G. C. (CN)
Bai, J. H. (CN)Source Title Advances in Space Research. - : Elsevier - ISSN 0273-1177
Roč. 48, - (2011), s. 2016-2022Number of pages 7 s. Language eng - English Country GB - United Kingdom Keywords annual cycle ; total ozone ; trends in annual cycle ; long–term trends Subject RIV DG - Athmosphere Sciences, Meteorology R&D Projects ME10077 GA MŠMT - Ministry of Education, Youth and Sports (MEYS) GAP209/10/1792 GA ČR - Czech Science Foundation (CSF) CEZ AV0Z30420517 - UFA-U, BC-A (2005-2011) UT WOS 000296998300009 DOI 10.1016/j.asr.2011.07.010 Annotation This paper deals with the behavior of the annual cycle of total ozone (ACO3) and its amplitude (O3AMP) in the latitudinal belt from 20° N to 60° N. The prominent feature of the O3AMP spatial pattern is the sharp maximum over the north-east coast of Asia. Regarding temporal evolution of O3AMP we detected distinct negative trend in the period of 1979-1995 which is caused by stronger negative trend of maxima than the negative trend of minima in ACO3. In the period 1995-2008 we found the positive trend of ACO3 in most regions due to stronger positive trend of maxima than that of minima in ACO3 in the middle latitudes (especially over the central and northern Europe and the north-east Asia). In the lower latitudes a weak negative trend of O3AMP was identified and linked to weaker positive trend of maxima than positive trend of minima in ACO3. The behavior of the temporal trends was linked to the changes in Brewer-Dobson circulation and to the trends of tropopause pressure. Workplace Institute of Atmospheric Physics Contact Kateřina Adamovičová, adamovicova@ufa.cas.cz, Tel.: 272 016 012 ; Kateřina Potužníková, kaca@ufa.cas.cz, Tel.: 272 016 019 Year of Publishing 2012 Electronic address http://www.sciencedirect.com/science/article/pii/S0273117711005436
Number of the records: 1