Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations

The first tropospheric and stratospheric (4 to 33 km) BrO profile is presented for the inner tropics derived from balloon-borne DOAS (Differential Optical Absorption Spectroscopy) measurements. In combination with photochemical modelling, total stratospheric inorganic bromine (Br<sub>y...

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Main Authors: M. Dorf, A. Butz, C. Camy-Peyret, M. P. Chipperfield, L. Kritten, K. Pfeilsticker
Format: Article
Language:English
Published: Copernicus Publications 2008-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/8/7265/2008/acp-8-7265-2008.pdf
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spelling doaj-483e46c3b0764664b4039c6de827bda02020-11-24T22:47:51ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242008-12-0182372657271Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observationsM. DorfA. ButzC. Camy-PeyretM. P. ChipperfieldL. KrittenK. PfeilstickerThe first tropospheric and stratospheric (4 to 33 km) BrO profile is presented for the inner tropics derived from balloon-borne DOAS (Differential Optical Absorption Spectroscopy) measurements. In combination with photochemical modelling, total stratospheric inorganic bromine (Br<sub>y</sub>) is deduced to be (21.5±2.5) ppt in 4.5-year-old air, probed in 2005. We derive a total contribution of (5.2±2.5) ppt from brominated very short-lived substances and inorganic product gases to stratospheric Br<sub>y</sub> Tropospheric BrO was found to be <1 ppt. Our results are compared to two 3-D CTM SLIMCAT model runs, which differ in the lifetime of the bromine source gases, affecting the vertical distribution of Br<sub>y</sub> in the lower stratosphere. Bromine source gas measurements performed 10 days earlier Laube et al., 2008, indicate a lower Br<sub>y</sub> of (17.5±0.4) ppt. Potential reasons for this discrepancy are discussed. http://www.atmos-chem-phys.net/8/7265/2008/acp-8-7265-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author M. Dorf
A. Butz
C. Camy-Peyret
M. P. Chipperfield
L. Kritten
K. Pfeilsticker
spellingShingle M. Dorf
A. Butz
C. Camy-Peyret
M. P. Chipperfield
L. Kritten
K. Pfeilsticker
Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
Atmospheric Chemistry and Physics
author_facet M. Dorf
A. Butz
C. Camy-Peyret
M. P. Chipperfield
L. Kritten
K. Pfeilsticker
author_sort M. Dorf
title Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
title_short Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
title_full Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
title_fullStr Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
title_full_unstemmed Bromine in the tropical troposphere and stratosphere as derived from balloon-borne BrO observations
title_sort bromine in the tropical troposphere and stratosphere as derived from balloon-borne bro observations
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2008-12-01
description The first tropospheric and stratospheric (4 to 33 km) BrO profile is presented for the inner tropics derived from balloon-borne DOAS (Differential Optical Absorption Spectroscopy) measurements. In combination with photochemical modelling, total stratospheric inorganic bromine (Br<sub>y</sub>) is deduced to be (21.5±2.5) ppt in 4.5-year-old air, probed in 2005. We derive a total contribution of (5.2±2.5) ppt from brominated very short-lived substances and inorganic product gases to stratospheric Br<sub>y</sub> Tropospheric BrO was found to be <1 ppt. Our results are compared to two 3-D CTM SLIMCAT model runs, which differ in the lifetime of the bromine source gases, affecting the vertical distribution of Br<sub>y</sub> in the lower stratosphere. Bromine source gas measurements performed 10 days earlier Laube et al., 2008, indicate a lower Br<sub>y</sub> of (17.5±0.4) ppt. Potential reasons for this discrepancy are discussed.
url http://www.atmos-chem-phys.net/8/7265/2008/acp-8-7265-2008.pdf
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