The ozone recovery in the NH extratropics: The trend analyses of the SBUV/SBUV-2 merged ozone data in the 1979―2012 period
- Author
- KRZYSCIN, Janusz W1
[1] Institute of Geophysics, Polish Academy of Sciences, 64 Księcia Janusza Street, 01-452 Warsaw, Poland - Source
Atmospheric environment (1994). 2014, Vol 98, pp 17-24, 8 p ; ref : 3/4 p
- ISSN
- 1352-2310
- Scientific domain
- Environment; Climatology, meteorology; Pollution; Toxicology
- Publisher
- Elsevier, Kidlington
- Publication country
- United Kingdom
- Document type
- Article
- Language
- English
- Author keyword
- Atmospheric ozone Recovery Stratospheric dynamics and chemistry
- Keyword (fr)
- Analyse série temporelle Analyse tendance Couche ozone Evaluation performance Hémisphère Nord Oxydant photochimique Ozone Politique environnement Stratosphère Trou ozone Zone extratropicale
- Keyword (en)
- time series analysis trend-surface analysis Ozone layer Performance evaluation Northern Hemisphere Photochemical oxidants ozone Environmental policy stratosphere Ozone holes Extratropical zone
- Keyword (es)
- Análisis tendencia Evaluación prestación Hemisferio norte Ozono Política medio ambiente Estratosfera Zona extratropical
- Classification
- Pascal
- 001 Exact sciences and technology / 001E Earth, ocean, space / 001E02 External geophysics / 001E02H Physics of the high neutral atmosphere / 001E02H02 Atmospheric composition. Chemical and photochemical reactions
- Discipline
- External geophysics
- Origin
- Inist-CNRS
- Database
- PASCAL
- INIST identifier
- 28866565
Sauf mention contraire ci-dessus, le contenu de cette notice bibliographique peut être utilisé dans le cadre d’une licence CC BY 4.0 Inist-CNRS / Unless otherwise stated above, the content of this bibliographic record may be used under a CC BY 4.0 licence by Inist-CNRS / A menos que se haya señalado antes, el contenido de este registro bibliográfico puede ser utilizado al amparo de una licencia CC BY 4.0 Inist-CNRS
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DOI
10.1016/j.atmosenv.2014.08.029 
https://dx.doi.org/10.1016/j.atmosenv.2014.08.029
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