Please use this identifier to cite or link to this item: http://hdl.handle.net/2248/5601
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dc.contributor.authorShantikumar, N. S-
dc.date.accessioned2011-10-25T14:07:28Z-
dc.date.available2011-10-25T14:07:28Z-
dc.date.issued2011-10-
dc.identifier.citationJournal of Atmospheric and Solar-Terrestrial Physics, Vol. 73, No. 16, pp. 2305-2313en
dc.identifier.urihttp://hdl.handle.net/2248/5601-
dc.descriptionRestricted Accessen
dc.description.abstractLong-term trend of total column ozone at high altitude region in Ladakh is studied, using a total ozone mapping spectrometer and an ozone monitoring instrument during 1979–2008. In the region, total ozone exhibits seasonality with maximum in spring and minimum in autumn. The decreasing trend of total ozone was found as −2.51±0.45% per decade with 95% confidence level in the region. Ozone deficiency in the Ladakh region is strongest (−33.9 DU at Hanle) in May and weakest (−11.5 DU at Hanle) in January–February. In the study, the solar maximum in 1990 is in phase with ozone maximum, while ozone variation lags in phase with the 1980 and 2000 solar maxima. However, a significant correlation between total ozone and sunspot number is achieved in the westerly phase of quasi-biennial oscillation during spring season. Decreasing trend of ozone in the region is correlating well with the cooling rate in the lower stratosphere.en
dc.language.isoenen
dc.publisherElsevier B.V.en
dc.relation.urihttp://dx.doi.org/10.1016/j.jastp.2011.06.015en
dc.rights© Elsevier B.V.en
dc.subjectOzone monitoring instrumenten
dc.subjectTotal column ozoneen
dc.subjectSolar maximaen
dc.subjectQuasi-biennial oscillationen
dc.titleVariability of sunspot cycle QBO and total ozone over high altitude Western Himalayan regionsen
dc.typeArticleen
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