Please use this identifier to cite or link to this item: https://repositorio.uca.edu.ar/handle/123456789/9518
Título : Reactive bromine in the low troposphere of Antarctica : estimations at two research sites
Autor : Prados Roman, Cristina 
Gómez Martín, Laura 
Puentedura, Olga 
Navarro Comas, Mónica 
Iglesias, Javier 
De Mingo, José Ramón 
Pérez, Manuel 
Ochoa, Héctor 
Barlasina, María Helena 
Carbajal, Gerardo 
Yela, Margarita 
Palabras clave : BROMOTROPOSFERAANTARTIDA
Fecha de publicación : 2018
Editorial : European Geosciences Union
Cita : Prados Roman, C. et. al. Reactive bromine in the low troposphere of Antarctica : estimations at two research sites [en línea]. Atmospheric Chemistry and Physics. 2018, 18. doi:10.5194/acp-18-8549-2018 Disponible en: https://repositorio.uca.edu.ar/handle/123456789/9518
Resumen : Abstract: For decades, reactive halogen species (RHSs) have been the subject of detailed scientific research due to their influence on the oxidizing capacity of the atmosphere and on the climate. From the RHSs, those containing bromine are of particular interest in the polar troposphere as a result of their link to ozone-depletion events (ODEs) and to the perturbation of the cycle of toxic mercury, for example. Given its remoteness and related limited accessibility compared to the Arctic region, the RHSs in the Antarctic troposphere are still poorly characterized. This work presents ground-based observations of tropospheric BrO from two different Antarctic locations: Marambio Base (64∘13′ S, 56∘37′ W) and Belgrano II Base (77∘52′ S, 34∘7′ W) during the sunlit period of 2015. By means of MAX-DOAS (Multi-axis Differential Optical Absorption Spectroscopy) measurements of BrO performed from the two research sites, the seasonal variation in this reactive trace gas is described along with its vertical and geographical distribution in the Antarctic environment. Results show an overall vertical profile of BrO mixing ratio decreasing with altitude, with a median value of 1.6 pmol mol−1 in the lowest layers of the troposphere. Additionally, observations show that the polar sunrise triggers a geographical heterogeneous increase in bromine content in the Antarctic troposphere yielding a maximum BrO at Marambio (26 pmol mol−1), amounting to 3-fold the values observed at Belgrano at dawn. Data presented herein are combined with previous studies and ancillary data to update and expand our knowledge of the geographical and vertical distribution of BrO in the Antarctic troposphere, revealing Marambio as one of the locations with the highest BrO reported so far in Antarctica. Furthermore, the observations gathered during 2015 serve as a proxy to investigate the budget of reactive bromine (BrOx = Br + BrO) and the bromine-mediated ozone loss rate in the Antarctic troposphere.
URI : https://repositorio.uca.edu.ar/handle/123456789/9518
ISSN : 1680-7316 (impreso)
1680-7324 (online)
Disciplina: INGENIERIA AMBIENTAL
DOI: 10.5194/acp-18-8549-2018
Derechos: Acceso abierto
Appears in Collections:Artículos

Files in This Item:
File Description SizeFormat
reactive-bromine-low-troposphere.pdf10,54 MBAdobe PDFThumbnail
View/Open
Show full item record

Page view(s)

61
checked on Feb 28, 2021

Download(s)

43
checked on Feb 28, 2021

Google ScholarTM

Check


Altmetric


This item is licensed under a Creative Commons License Creative Commons