Please use this identifier to cite or link to this item: http://hdl.handle.net/20.500.11765/7043
Hemispheric asymmetry in stratospheric NO2 trends
Title: Hemispheric asymmetry in stratospheric NO2 trends
Authors: Yela, MargaritaGil-Ojeda, ManuelNavarro Comas, MónicaGonzález-Bartolome, DavidPuentedura, OlgaFunke, BerndIglesias, J.Rodríguez, SantiagoGarcía Rodríguez, Omaira Elena ORCID RESEARCHERID Ochoa, HectorDeferrari, Guillermo
Keywords: Nitrogen dioxide; Stratospheric trends; Ozone; Differential optical absorption spectroscopy (DOAS); Dióxido de nitrógeno; Ozono; Espectroscopía Óptica de Absorción Diferencial
Issue Date: 2017
Publisher: European Geosciences Union
Citation: Atmospheric Chemistry and Physics. 2017, 17(21), p. 13373–13389
Publisher version: https://dx.doi.org/10.5194/acp-17-13373-2017
Abstract: Over 20 years of stratospheric NO2 vertical column density (VCD) data from ground-based zenith DOAS spectrometers were used for trend analysis, specifically, via multiple linear regression. Spectrometers from the Network for the Detection of Atmospheric Composition Change (NDACC) cover the subtropical latitudes in the Northern Hemisphere (Izaña, 28° N), the southern Subantarctic (Ushuaia, 55° S) and Antarctica (Marambio, 64° S, and Belgrano, 78° S). The results show that for the period 1993–2014, a mean positive decadal trend of +8.7 % was found in the subtropical Northern Hemisphere stations, and negative decadal trends of −8.7 and −13.8 % were found in the Southern Hemisphere at Ushuaia and Marambio, respectively; all trends are statistically significant at 95 %. Belgrano only shows a significant decadal trend of −11.3 % in the summer/autumn period. Most of the trends result from variations after 2005. The trend in the diurnal build-up per hour (DBU) was used to estimate the change in the rate of N2O5 conversion to NO2 during the day. With minor differences, the results reproduce those obtained for NO2. The trends computed for individual months show large month-to-month variability. At Izaña, the maximum occurs in December (+13.1 %), dropping abruptly to lower values in the first part of the year. In the Southern Hemisphere, the polar vortex dominates the monthly distributions of the trends. At Marambio, the maximum occurs in mid-winter (−21 %), whereas at the same time, the Ushuaia trend is close to its annual minimum (−7 %). The large difference in the trends at these two relatively close stations suggests a vortex shift towards the Atlantic/South American area over the past few years. Finally, the hemispheric asymmetry obtained in this work is discussed in the framework of the results obtained by previous works that considered tracer analysis and Brewer–Dobson circulation. The results obtained here provide evidence that the NO2 produced by N2O decomposition is not the only cause of the observed trend in the stratosphere and support recent publications pointing to a dynamical redistribution starting in the past decade.
Sponsorship : Long-term measurements were made possible thanks to the funding provided by EU Framework programme NORS (FP7/2007-2013 under grant agreement no. 284421) and Spanish R+D Plan projects AMISOC (CGL2011-24891), AVATAR (CGL2014-55230-R), VIOLIN (CGL2010-20353) and HELADO (CTM2013-41311-P). The trend analysis was programmed with the GNU OCTAVE version 4.2.0 free software.
URI: http://hdl.handle.net/20.500.11765/7043
ISSN: 1680-7316
1680-7324
Appears in Collections:Artículos científicos 2015-2018


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