FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006558037> ?p ?o ?g. }

• W2006558037 endingPage "5008" @default.
• W2006558037 startingPage "4985" @default.
• W2006558037 abstract "Abstract. Trends in ozone columns and vertical distributions were calculated for the period 1979–2004 based on the ozone data set CATO (Candidoz Assimilated Three-dimensional Ozone) using a multiple linear regression model. CATO has been reconstructed from TOMS, GOME and SBUV total column ozone observations in an equivalent latitude and potential temperature framework and offers a pole to pole coverage of the stratosphere on 15 potential temperature levels. The regression model includes explanatory variables describing the influence of the quasi-biennial oscillation (QBO), volcanic eruptions, the solar cycle, the Brewer-Dobson circulation, Arctic ozone depletion, and the increase in stratospheric chlorine. The effects of displacements of the polar vortex and jet streams due to planetary waves, which may significantly affect trends at a given geographical latitude, are eliminated in the equivalent latitude framework. The QBO shows a strong signal throughout most of the lower stratosphere with peak amplitudes in the tropics of the order of 10–20% (peak to valley). The eruption of Pinatubo led to annual mean ozone reductions of 15–25% between the tropopause and 23 km in northern mid-latitudes and to similar percentage changes in the southern hemisphere but concentrated at altitudes below 17 km. Stratospheric ozone is elevated over a broad latitude range by up to 5% during solar maximum compared to solar minimum, the largest increase being observed around 30 km. This is at a lower altitude than reported previously, and no negative signal is found in the tropical lower stratosphere. The Brewer-Dobson circulation shows a dominant contribution to interannual variability at both high and low latitudes and accounts for some of the ozone increase seen in the northern hemisphere since the mid-1990s. Arctic ozone depletion significantly affects the high northern latitudes between January and March and extends its influence to the mid-latitudes during later months. The vertical distribution of the ozone trend shows distinct negative trends at about 18 km in the lower stratosphere with largest declines over the poles, and above 35 km in the upper stratosphere. A narrow band of large negative trends extends into the tropical lower stratosphere. Assuming that the observed negative trend before 1995 continued to 2004 cannot explain the ozone changes since 1996. A model accounting for recent changes in equivalent effective stratospheric chlorine, aerosols and Eliassen-Palm flux, on the other hand, closely tracks ozone changes since 1995." @default.
• W2006558037 created "2016-06-24" @default.
• W2006558037 creator A5026127318 @default.
• W2006558037 creator A5045537234 @default.
• W2006558037 creator A5068941485 @default.
• W2006558037 creator A5080964622 @default.
• W2006558037 creator A5087702949 @default.
• W2006558037 date "2006-10-31" @default.
• W2006558037 modified "2023-10-13" @default.
• W2006558037 title "Variability and trends in total and vertically resolved stratospheric ozone based on the CATO ozone data set" @default.
• W2006558037 cites W1617743759 @default.
• W2006558037 cites W1964436263 @default.
• W2006558037 cites W1964625810 @default.
• W2006558037 cites W1968053224 @default.
• W2006558037 cites W1969128183 @default.
• W2006558037 cites W1971328808 @default.
• W2006558037 cites W1971991115 @default.
• W2006558037 cites W1972431979 @default.
• W2006558037 cites W1975242068 @default.
• W2006558037 cites W1986775482 @default.
• W2006558037 cites W1990466322 @default.
• W2006558037 cites W1995182760 @default.
• W2006558037 cites W1996748879 @default.
• W2006558037 cites W2001971406 @default.
• W2006558037 cites W2004447171 @default.
• W2006558037 cites W2005334558 @default.
• W2006558037 cites W2008343961 @default.
• W2006558037 cites W2014862170 @default.
• W2006558037 cites W2015111757 @default.
• W2006558037 cites W2017887707 @default.
• W2006558037 cites W2018043695 @default.
• W2006558037 cites W2019675651 @default.
• W2006558037 cites W2020378808 @default.
• W2006558037 cites W2020967789 @default.
• W2006558037 cites W2021758596 @default.
• W2006558037 cites W2024800955 @default.
• W2006558037 cites W2025560484 @default.
• W2006558037 cites W2030957302 @default.
• W2006558037 cites W2031124595 @default.
• W2006558037 cites W2035807572 @default.
• W2006558037 cites W2037861133 @default.
• W2006558037 cites W2042322145 @default.
• W2006558037 cites W2042943378 @default.
• W2006558037 cites W2042950462 @default.
• W2006558037 cites W2043223750 @default.
• W2006558037 cites W2045045432 @default.
• W2006558037 cites W2055873026 @default.
• W2006558037 cites W2057336394 @default.
• W2006558037 cites W2058179313 @default.
• W2006558037 cites W2061936417 @default.
• W2006558037 cites W2063129630 @default.
• W2006558037 cites W2071641166 @default.
• W2006558037 cites W2075659946 @default.
• W2006558037 cites W2078736748 @default.
• W2006558037 cites W2081281724 @default.
• W2006558037 cites W2081999344 @default.
• W2006558037 cites W2088741783 @default.
• W2006558037 cites W2095329169 @default.
• W2006558037 cites W2096233207 @default.
• W2006558037 cites W2096814380 @default.
• W2006558037 cites W2098405759 @default.
• W2006558037 cites W2102569455 @default.
• W2006558037 cites W2108256342 @default.
• W2006558037 cites W2112632251 @default.
• W2006558037 cites W2117082770 @default.
• W2006558037 cites W2118934803 @default.
• W2006558037 cites W2127290989 @default.
• W2006558037 cites W2131143266 @default.
• W2006558037 cites W2140744430 @default.
• W2006558037 cites W2147382978 @default.
• W2006558037 cites W2154123106 @default.
• W2006558037 cites W2165257577 @default.
• W2006558037 cites W2167051621 @default.
• W2006558037 cites W2171178947 @default.
• W2006558037 cites W2171248599 @default.
• W2006558037 cites W2180641895 @default.
• W2006558037 doi "https://doi.org/10.5194/acp-6-4985-2006" @default.
• W2006558037 hasPublicationYear "2006" @default.
• W2006558037 type Work @default.
• W2006558037 sameAs 2006558037 @default.
• W2006558037 citedByCount "53" @default.
• W2006558037 countsByYear W20065580372012 @default.
• W2006558037 countsByYear W20065580372013 @default.
• W2006558037 countsByYear W20065580372014 @default.
• W2006558037 countsByYear W20065580372015 @default.
• W2006558037 countsByYear W20065580372016 @default.
• W2006558037 countsByYear W20065580372017 @default.
• W2006558037 countsByYear W20065580372018 @default.
• W2006558037 countsByYear W20065580372019 @default.
• W2006558037 countsByYear W20065580372021 @default.
• W2006558037 countsByYear W20065580372022 @default.
• W2006558037 countsByYear W20065580372023 @default.
• W2006558037 crossrefType "journal-article" @default.
• W2006558037 hasAuthorship W2006558037A5026127318 @default.
• W2006558037 hasAuthorship W2006558037A5045537234 @default.
• W2006558037 hasAuthorship W2006558037A5068941485 @default.
• W2006558037 hasAuthorship W2006558037A5080964622 @default.
• W2006558037 hasAuthorship W2006558037A5087702949 @default.

• next