TY - JOUR
T1 - Modelling the impacts of iodine chemistry on the northern Indian Ocean marine boundary layer
AU - Mahajan, Anoop S.
AU - Li, Qinyi
AU - Inamdar, Swaleha
AU - Ram, Kirpa
AU - Badia, Alba
AU - Saiz-Lopez, Alfonso
N1 - Publisher Copyright:
© 2021 Copernicus GmbH. All rights reserved.
PY - 2021/6/3
Y1 - 2021/6/3
N2 - Recent observations have shown the ubiquitous presence of iodine oxide (IO) in the Indian Ocean marine boundary layer (MBL). In this study, we use the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem version 3.7.1), including halogen (Br, Cl, and I) sources and chemistry, to quantify the impacts of the observed levels of iodine on the chemical composition of the MBL. The model results show that emissions of inorganic iodine species resulting from the deposition of ozone (span classCombining double low line"inline-formula"O3/span) on the sea surface are needed to reproduce the observed levels of IO, although the current parameterizations overestimate the atmospheric concentrations. After reducing the inorganic emissions by 40 %, a reasonable match with cruise-based observations is found, with the model predicting values between 0.1 and 1.2 span classCombining double low line"inline-formula"pptv/span across the model domain MBL. A strong seasonal variation is also observed, with lower iodine concentrations predicted during the monsoon period, when clean oceanic air advects towards the Indian subcontinent, and higher iodine concentrations predicted during the winter period, when polluted air from the Indian subcontinent increases the ozone concentrations in the remote MBL. The results show that significant changes are caused by the inclusion of iodine chemistry, with iodine-catalysed reactions leading to regional changes of up to 25 % in span classCombining double low line"inline-formula"O3/span, 50 % in nitrogen oxides (NO and span classCombining double low line"inline-formula"NO2/span), 15 % in hydroxyl radicals (OH), 25 % in hydroperoxyl radicals (span classCombining double low line"inline-formula"HO2/span), and up to a 50 % change in the nitrate radical (span classCombining double low line"inline-formula"NO3/span), with lower mean values across the domain. Most of the large relative changes are observed in the open-ocean MBL, although iodine chemistry also affects the chemical composition in the coastal environment and over the Indian subcontinent. These results show the importance of including iodine chemistry in modelling the atmosphere in this region./
AB - Recent observations have shown the ubiquitous presence of iodine oxide (IO) in the Indian Ocean marine boundary layer (MBL). In this study, we use the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem version 3.7.1), including halogen (Br, Cl, and I) sources and chemistry, to quantify the impacts of the observed levels of iodine on the chemical composition of the MBL. The model results show that emissions of inorganic iodine species resulting from the deposition of ozone (span classCombining double low line"inline-formula"O3/span) on the sea surface are needed to reproduce the observed levels of IO, although the current parameterizations overestimate the atmospheric concentrations. After reducing the inorganic emissions by 40 %, a reasonable match with cruise-based observations is found, with the model predicting values between 0.1 and 1.2 span classCombining double low line"inline-formula"pptv/span across the model domain MBL. A strong seasonal variation is also observed, with lower iodine concentrations predicted during the monsoon period, when clean oceanic air advects towards the Indian subcontinent, and higher iodine concentrations predicted during the winter period, when polluted air from the Indian subcontinent increases the ozone concentrations in the remote MBL. The results show that significant changes are caused by the inclusion of iodine chemistry, with iodine-catalysed reactions leading to regional changes of up to 25 % in span classCombining double low line"inline-formula"O3/span, 50 % in nitrogen oxides (NO and span classCombining double low line"inline-formula"NO2/span), 15 % in hydroxyl radicals (OH), 25 % in hydroperoxyl radicals (span classCombining double low line"inline-formula"HO2/span), and up to a 50 % change in the nitrate radical (span classCombining double low line"inline-formula"NO3/span), with lower mean values across the domain. Most of the large relative changes are observed in the open-ocean MBL, although iodine chemistry also affects the chemical composition in the coastal environment and over the Indian subcontinent. These results show the importance of including iodine chemistry in modelling the atmosphere in this region./
UR - http://www.scopus.com/inward/record.url?scp=85107412353&partnerID=8YFLogxK
U2 - 10.5194/acp-21-8437-2021
DO - 10.5194/acp-21-8437-2021
M3 - Article
AN - SCOPUS:85107412353
SN - 1680-7316
VL - 21
SP - 8437
EP - 8454
JO - Atmospheric Chemistry and Physics
JF - Atmospheric Chemistry and Physics
IS - 11
ER -