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• W2096233207 endingPage "1180" @default.
• W2096233207 startingPage "1165" @default.
• W2096233207 abstract "Abstract. Global total ozone measurements from various satellite instruments such as SBUV, TOMS, and GOME show an increase in zonal mean total ozone at northern hemispheric (NH) mid to high latitudes since the mid-nineties. This increase could be expected from the peaking and start of decline in the effective stratospheric halogen loading, but the rather rapid increase observed in NH zonal mean total ozone suggests that another physical mechanism such as winter planetary wave activity has increased which has led to higher stratospheric Arctic temperatures. This has enhanced ozone transport into higher latitudes in recent years as part of the residual circulation and at the same time reduced the frequency of cold Arctic winters with enhanced polar ozone loss. Results from various multi-variate linear regression analyses using SBUV V8 total ozone with explanatory variables such as a linear trend or, alternatively, EESC (equivalent effective stratospheric chlorine) and on the other hand planetary wave driving (eddy heat flux) or, alternatively, polar ozone loss (PSC volume) in addition to proxies for stratospheric aerosol loading, QBO, and solar cycle, all considered to be main drivers for ozone variability, are presented. It is shown that the main contribution to the recent increase in NH total ozone is from the combined effect of rising tropospheric driven planetary wave activity associated with reduced polar ozone loss at high latitudes as well as increasing solar activity. This conclusion can be drawn regardless of the use of linear trend or EESC terms in our statistical model. It is also clear that more years of data will be needed to further improve our estimates of the relative contributions of the individual processes to decadal ozone variability. The question remains if the observed increase in planetary wave driving is part of natural decadal atmospheric variability or will persist. If the latter is the case, it could be interpreted as a possible signature of climate change." @default.
• W2096233207 created "2016-06-24" @default.
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• W2096233207 date "2006-04-13" @default.
• W2096233207 modified "2023-10-11" @default.
• W2096233207 title "On the possible causes of recent increases in northern hemispheric total ozone from a statistical analysis of satellite data from 1979 to 2003" @default.
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• W2096233207 cites W1575534835 @default.
• W2096233207 cites W172300334 @default.
• W2096233207 cites W1818398520 @default.
• W2096233207 cites W1965534149 @default.
• W2096233207 cites W1971868152 @default.
• W2096233207 cites W1977052563 @default.
• W2096233207 cites W1977343561 @default.
• W2096233207 cites W1977489501 @default.
• W2096233207 cites W1977662333 @default.
• W2096233207 cites W1982127484 @default.
• W2096233207 cites W1986184913 @default.
• W2096233207 cites W1986775482 @default.
• W2096233207 cites W1987770728 @default.
• W2096233207 cites W1992450374 @default.
• W2096233207 cites W1993185787 @default.
• W2096233207 cites W1997808327 @default.
• W2096233207 cites W2000046838 @default.
• W2096233207 cites W2001656621 @default.
• W2096233207 cites W2003266253 @default.
• W2096233207 cites W2003926579 @default.
• W2096233207 cites W2004141141 @default.
• W2096233207 cites W2004930136 @default.
• W2096233207 cites W2008343961 @default.
• W2096233207 cites W2010170520 @default.
• W2096233207 cites W2014931100 @default.
• W2096233207 cites W2017887707 @default.
• W2096233207 cites W2018043695 @default.
• W2096233207 cites W2019594051 @default.
• W2096233207 cites W2020378808 @default.
• W2096233207 cites W2022440867 @default.
• W2096233207 cites W2024632043 @default.
• W2096233207 cites W2025415734 @default.
• W2096233207 cites W2028489075 @default.
• W2096233207 cites W2029291699 @default.
• W2096233207 cites W2030842204 @default.
• W2096233207 cites W2030957302 @default.
• W2096233207 cites W2032394781 @default.
• W2096233207 cites W2034910289 @default.
• W2096233207 cites W2038660920 @default.
• W2096233207 cites W2042322145 @default.
• W2096233207 cites W2042950462 @default.
• W2096233207 cites W2043223750 @default.
• W2096233207 cites W2049127999 @default.
• W2096233207 cites W2052035096 @default.
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• W2096233207 cites W2058179313 @default.
• W2096233207 cites W2064817522 @default.
• W2096233207 cites W2078736748 @default.
• W2096233207 cites W2081281724 @default.
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• W2096233207 cites W2117082770 @default.
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• W2096233207 doi "https://doi.org/10.5194/acp-6-1165-2006" @default.
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