Research output: Contribution to Journal/Magazine › Journal article › peer-review
Research output: Contribution to Journal/Magazine › Journal article › peer-review
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TY - JOUR
T1 - Reaction between CH3O2 and BrO Radicals
T2 - a new source of upper troposphere lower stratosphere hydroxyl radicals
AU - Shallcross, Dudley E.
AU - Leather, Kimberley E.
AU - Bacak, Asan
AU - Xiao, Ping
AU - Lee, Edmond P. F.
AU - Ng, Maggie
AU - Mok, Daniel K. W.
AU - Dyke, John M.
AU - Hossaini, Ryan
AU - Chipperfield, Martyn P.
AU - Khan, M. Anwar H.
AU - Percival, Carl J.
PY - 2015/5/14
Y1 - 2015/5/14
N2 - Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposphere are often underestimated by models, leading to the assertion that there are missing sources. Here we report laboratory studies of the kinetics and products of the reaction between CH3O2 and BrO radicals that shows that this could be an important new source of hydroxyl radicals:BrO + CH3O2 --> products (1). The temperature dependent value in Arrhenius form of k(T) is k(1) = (2.42(-0.72)(+1.02)) X 10(-14) exp[(1617 +/- 94)/T] cm(3) molecule(-1) s(-1). In addition, CH2OO and HOBr are believed to he the major products. Global model results suggest that the decomposition of H2COO to form OH could lead to an enhancement in OH of up to 20% in mid-latitudes in the upper troposphere and in the lower stratosphere enhancements OH of 2-9% are inferred from model integrations. In addition, reaction 1 aids conversion of BrO to HOBr and slows polar ozone loss in the lower stratosphere.
AB - Over the last two decades it has emerged that measured hydroxyl radical levels in the upper troposphere are often underestimated by models, leading to the assertion that there are missing sources. Here we report laboratory studies of the kinetics and products of the reaction between CH3O2 and BrO radicals that shows that this could be an important new source of hydroxyl radicals:BrO + CH3O2 --> products (1). The temperature dependent value in Arrhenius form of k(T) is k(1) = (2.42(-0.72)(+1.02)) X 10(-14) exp[(1617 +/- 94)/T] cm(3) molecule(-1) s(-1). In addition, CH2OO and HOBr are believed to he the major products. Global model results suggest that the decomposition of H2COO to form OH could lead to an enhancement in OH of up to 20% in mid-latitudes in the upper troposphere and in the lower stratosphere enhancements OH of 2-9% are inferred from model integrations. In addition, reaction 1 aids conversion of BrO to HOBr and slows polar ozone loss in the lower stratosphere.
KW - IONIZATION MASS-SPECTROMETRY
KW - INTERMEDIATES CRI MECHANISM
KW - ACTIVE THERMOCHEMICAL TABLES
KW - GAS-PHASE
KW - PRESSURE-DEPENDENCE
KW - OZONE PHOTOCHEMISTRY
KW - BROMINE MONOXIDE
KW - BOUNDARY-LAYER
KW - TRACE GAS
KW - AB-INITIO
U2 - 10.1021/jp5108203
DO - 10.1021/jp5108203
M3 - Journal article
VL - 119
SP - 4618
EP - 4632
JO - Journal of Physical Chemistry A
JF - Journal of Physical Chemistry A
SN - 1089-5639
IS - 19
ER -