Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites
Dry deposition is an important removal mechanism for tropospheric ozone (O3). Currently, O3 deposition to oceans in atmospheric chemistry and transport models (ACTMs) is generally represented using constant surface uptake resistances. This occurs despite the role of solubility, waterside turbulence...
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ftunivwagenin:oai:library.wur.nl:wurpubs/585067 2024-04-28T08:07:12+00:00 Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites Barten, Johannes G.M. Ganzeveld, Laurens N. Steeneveld, Gert Jan Krol, Maarten C. 2021 application/pdf https://research.wur.nl/en/publications/role-of-oceanic-ozone-deposition-in-explaining-temporal-variabili https://doi.org/10.5194/acp-21-10229-2021 en eng https://edepot.wur.nl/550809 https://research.wur.nl/en/publications/role-of-oceanic-ozone-deposition-in-explaining-temporal-variabili doi:10.5194/acp-21-10229-2021 https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research Atmospheric Chemistry and Physics 21 (2021) 13 ISSN: 1680-7316 Life Science Article/Letter to editor 2021 ftunivwagenin https://doi.org/10.5194/acp-21-10229-2021 2024-04-03T15:01:56Z Dry deposition is an important removal mechanism for tropospheric ozone (O3). Currently, O3 deposition to oceans in atmospheric chemistry and transport models (ACTMs) is generally represented using constant surface uptake resistances. This occurs despite the role of solubility, waterside turbulence and O3 reacting with ocean water reactants such as iodide resulting in substantial spatiotemporal variability in O3 deposition and concentrations in marine boundary layers. We hypothesize that O3 deposition to the Arctic Ocean, having a relatively low reactivity, is overestimated in current models with consequences for the tropospheric concentrations, lifetime and long-range transport of O3. We investigate the impact of the representation of oceanic O3 deposition to the simulated magnitude and spatiotemporal variability in Arctic surface O3. We have integrated the Coupled Ocean-Atmosphere Response Experiment Gas transfer algorithm (COAREG) into the mesoscale meteorology and atmospheric chemistry model Polar-WRF-Chem (WRF) which introduces a dependence of O3 deposition on physical and biogeochemical drivers of oceanic O3 deposition. Also, we reduced the O3 deposition to sea ice and snow. Here, we evaluate WRF and CAMS reanalysis data against hourly averaged surface O3 observations at 25 sites (latitudes > 60° N). This is the first time such a coupled modeling system has been evaluated against hourly observations at pan-Arctic sites to study the sensitivity of the magnitude and temporal variability in Arctic surface O3 on the deposition scheme. We find that it is important to nudge WRF to the ECMWF ERA5 reanalysis data to ensure adequate meteorological conditions to evaluate surface O3. We show that the mechanistic representation of O3 deposition over oceans and reduced snow/ice deposition improves simulated Arctic O3 mixing ratios both in magnitude and temporal variability compared to the constant resistance approach. Using COAREG, O3 deposition velocities are in the order of 0.01 cm s-1 compared to ∼ 0.05 cm s-1 in ... Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Wageningen UR (University & Research Centre): Digital Library Atmospheric Chemistry and Physics 21 13 10229 10248 |
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English |
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Life Science |
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Life Science Barten, Johannes G.M. Ganzeveld, Laurens N. Steeneveld, Gert Jan Krol, Maarten C. Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
topic_facet |
Life Science |
description |
Dry deposition is an important removal mechanism for tropospheric ozone (O3). Currently, O3 deposition to oceans in atmospheric chemistry and transport models (ACTMs) is generally represented using constant surface uptake resistances. This occurs despite the role of solubility, waterside turbulence and O3 reacting with ocean water reactants such as iodide resulting in substantial spatiotemporal variability in O3 deposition and concentrations in marine boundary layers. We hypothesize that O3 deposition to the Arctic Ocean, having a relatively low reactivity, is overestimated in current models with consequences for the tropospheric concentrations, lifetime and long-range transport of O3. We investigate the impact of the representation of oceanic O3 deposition to the simulated magnitude and spatiotemporal variability in Arctic surface O3. We have integrated the Coupled Ocean-Atmosphere Response Experiment Gas transfer algorithm (COAREG) into the mesoscale meteorology and atmospheric chemistry model Polar-WRF-Chem (WRF) which introduces a dependence of O3 deposition on physical and biogeochemical drivers of oceanic O3 deposition. Also, we reduced the O3 deposition to sea ice and snow. Here, we evaluate WRF and CAMS reanalysis data against hourly averaged surface O3 observations at 25 sites (latitudes > 60° N). This is the first time such a coupled modeling system has been evaluated against hourly observations at pan-Arctic sites to study the sensitivity of the magnitude and temporal variability in Arctic surface O3 on the deposition scheme. We find that it is important to nudge WRF to the ECMWF ERA5 reanalysis data to ensure adequate meteorological conditions to evaluate surface O3. We show that the mechanistic representation of O3 deposition over oceans and reduced snow/ice deposition improves simulated Arctic O3 mixing ratios both in magnitude and temporal variability compared to the constant resistance approach. Using COAREG, O3 deposition velocities are in the order of 0.01 cm s-1 compared to ∼ 0.05 cm s-1 in ... |
format |
Article in Journal/Newspaper |
author |
Barten, Johannes G.M. Ganzeveld, Laurens N. Steeneveld, Gert Jan Krol, Maarten C. |
author_facet |
Barten, Johannes G.M. Ganzeveld, Laurens N. Steeneveld, Gert Jan Krol, Maarten C. |
author_sort |
Barten, Johannes G.M. |
title |
Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
title_short |
Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
title_full |
Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
title_fullStr |
Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
title_full_unstemmed |
Role of oceanic ozone deposition in explaining temporal variability in surface ozone at High Arctic sites |
title_sort |
role of oceanic ozone deposition in explaining temporal variability in surface ozone at high arctic sites |
publishDate |
2021 |
url |
https://research.wur.nl/en/publications/role-of-oceanic-ozone-deposition-in-explaining-temporal-variabili https://doi.org/10.5194/acp-21-10229-2021 |
genre |
Arctic Arctic Ocean Sea ice |
genre_facet |
Arctic Arctic Ocean Sea ice |
op_source |
Atmospheric Chemistry and Physics 21 (2021) 13 ISSN: 1680-7316 |
op_relation |
https://edepot.wur.nl/550809 https://research.wur.nl/en/publications/role-of-oceanic-ozone-deposition-in-explaining-temporal-variabili doi:10.5194/acp-21-10229-2021 |
op_rights |
https://creativecommons.org/licenses/by/4.0/ Wageningen University & Research |
op_doi |
https://doi.org/10.5194/acp-21-10229-2021 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
21 |
container_issue |
13 |
container_start_page |
10229 |
op_container_end_page |
10248 |
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1797576408575246336 |