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Chemically-induced total ozone column loss derived by comparing observations of total ozone with a chemical transport model calculation where ozone is treated as a chemically inert tracer. The observations are carried out with SAOZ UV-Visible spectrometers at high-latitude sites of the GAW-contribut...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.433.4135 2023-05-15T14:20:59+02:00 THULE The Pennsylvania State University CiteSeerX Archives 2006 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.433.4135 http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.433.4135 http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf text 2006 ftciteseerx 2016-01-08T04:48:26Z Chemically-induced total ozone column loss derived by comparing observations of total ozone with a chemical transport model calculation where ozone is treated as a chemically inert tracer. The observations are carried out with SAOZ UV-Visible spectrometers at high-latitude sites of the GAW-contributing Network for the Detection of Atmospheric Composition Change (NDACC). Although the 2005-06 Arctic stratospheric winter overall featured a weak vortex and was one of the mildest on record, low temperatures in December and January, combined with a displacement of the vortex towards sunlit latitudes resulted in significant ozone loss, although to a lesser extent than seen during cold Arctic winters. The plot is provided by Florence Goutail, Service d'A'éronomie, CNRS. Text Arctic Arctic Unknown Arctic |
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English |
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Chemically-induced total ozone column loss derived by comparing observations of total ozone with a chemical transport model calculation where ozone is treated as a chemically inert tracer. The observations are carried out with SAOZ UV-Visible spectrometers at high-latitude sites of the GAW-contributing Network for the Detection of Atmospheric Composition Change (NDACC). Although the 2005-06 Arctic stratospheric winter overall featured a weak vortex and was one of the mildest on record, low temperatures in December and January, combined with a displacement of the vortex towards sunlit latitudes resulted in significant ozone loss, although to a lesser extent than seen during cold Arctic winters. The plot is provided by Florence Goutail, Service d'A'éronomie, CNRS. |
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The Pennsylvania State University CiteSeerX Archives |
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2006 |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.433.4135 http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf |
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Arctic Arctic |
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Arctic Arctic |
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http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf |
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http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.433.4135 http://www.wmo.int/pages/prog/arep/gaw/ozone/documents/arctic-bulletin-2005-2006.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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1766293559423533056 |