|
Read Full Article (file size: 2063882 bytes) Cited by
JOURNAL OF GEOPHYSICAL RESEARCH,
VOL. 111,
D14301,
doi:10.1029/2005JD006479,
2006
Latitudinal and vertical distribution of bromine monoxide in the lower stratosphere from Scanning Imaging Absorption Spectrometer
for Atmospheric Chartography limb scattering measurements
C. E. Sioris
Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts, USA
L. J. Kovalenko
Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California, USA
C. A. McLinden
Meteorological Service of Canada, Environment Canada, Toronto, Ontario, Canada
R. J. Salawitch
Jet Propulsion Laboratory, Pasadena, California, USA
M. Van Roozendael
Belgian Institute for Space Aeronomy, Brussels, Belgium
F. Goutail
Service d'Aéronomie, Centre National de la Recherche Scientifique, Verrières-le-Buisson, France
M. Dorf
Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
K. Pfeilsticker
Institute of Environmental Physics, University of Heidelberg, Heidelberg, Germany
K. Chance
Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts, USA
C. von Savigny
Institute of Environmental Physics, University of Bremen, Bremen, Germany
X. Liu
Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts, USA
T. P. Kurosu
Harvard-Smithsonian Center for Astrophysics, Cambridge, Massachusetts, USA
J.-P. Pommereau
Service d'Aéronomie, Centre National de la Recherche Scientifique, Verrières-le-Buisson, France
H. Bösch
Jet Propulsion Laboratory, Pasadena, California, USA
J. Frerick
European Space Agency/European Space Research and Technology Centre, Noordwijk, Netherlands
Abstract
Vertical profiles of stratospheric bromine monoxide (BrO) in the 15–30 km range are retrieved from SCIAMACHY limb scatter
data over the globe. First validation comparisons with the balloon-borne SAOZ-BrO and LPMA/DOAS instruments indicate retrieval
biases of ∼20% or less. Propagated spectral fitting uncertainties lead to a precision approaching ∼25% on a 2 km grid at 25
km. This worsens at higher altitudes because of reduced signal and at lower altitudes because of the reduced penetrability
of the atmosphere. In terms of volume mixing ratio (VMR), the single profile precision increases from ∼4 pptv at 17 km to
∼8 pptv at 27 km. Repeatability, an alternative indicator of precision, is 2–3 pptv for SCIAMACHY retrievals and independent
of altitude. The BrO stratospheric number density peak generally lies 5 ± 2 km above the tropopause. In the tropics, the stratospheric
BrO VMR generally increases with increasing altitude. The observed stratospheric BrO global distribution is generally consistent
with previous balloon measurements but does not agree well with results of a model that uses Bry inferred only from the observed breakdown of long-lived bromoalkanes (i.e., methyl bromide and halons). We find best agreement
with the observed vertical and latitudinal distribution of BrO for model results that include an 8.4 ± 2 pptv contribution
to stratospheric Bry, most of which is expected from the breakdown of VSL (very short lived) bromocarbons, in addition to the ∼16 pptv contribution
from longer-lived sources. This suggests that stratospheric Bry exceeds 20 pptv. Profiles of Bry profiles derived from the balloon measurements of BrO also suggest Bry is in excess of 20 pptv, but the uncertainty and variability of these results do not allow us to definitively rule out this
concentration. We find typical BrO VMRs of ∼4 pptv at 15 km in the tropical tropopause layer, suggesting that a significant
portion of the bromine from VSL bromoalkane sources may be carried across the tropopause in the form of inorganic decomposition
products. We discuss a variety of VSL bromocarbons species that may be contributing to the elevated concentrations of stratospheric
BrO.
Received 13
July
2005;
accepted 24
April
2006;
published 19
July
2006.
Keywords: inorganic bromine;
stratospheric;
limb scattering.
Index Terms: 3360 Atmospheric Processes: Remote sensing; 0340 Atmospheric Composition and Structure: Middle atmosphere: composition and chemistry; 0317 Atmospheric Composition and Structure: Chemical kinetic and photochemical properties.
Read Full Article (file size: 2063882 bytes) Cited by
Citation: Sioris, C. E., et al.
(2006),
Latitudinal and vertical distribution of bromine monoxide in the lower stratosphere from Scanning Imaging Absorption Spectrometer
for Atmospheric Chartography limb scattering measurements,
J. Geophys. Res.,
111,
D14301,
doi:10.1029/2005JD006479.
Copyright 2006 by the American Geophysical Union.
|