Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer

The chemical evolution of the exhaust plumes of ocean-going ships in the cloud-free marine boundary layer is examined with a box model. Dilution of the ship plume via entrainment of background air was treated as in studies of aircraft emissions and was found to be a very important process that sig...

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Main Authors: R. von Glasow, M. G. Lawrence, R. Sander, P. J. Crutzen
Format: Article
Language:English
Published: Copernicus Publications 2003-01-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/3/233/2003/acp-3-233-2003.pdf
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spelling doaj-66a6fa50645640d9ba5b004cab72a7b62020-11-24T22:38:24ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242003-01-0131233250Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layerR. von GlasowR. von GlasowM. G. LawrenceR. SanderP. J. CrutzenP. J. CrutzenThe chemical evolution of the exhaust plumes of ocean-going ships in the cloud-free marine boundary layer is examined with a box model. Dilution of the ship plume via entrainment of background air was treated as in studies of aircraft emissions and was found to be a very important process that significantly alters model results. We estimated the chemical lifetime (defined as the time when differences between plume and background air are reduced to 5% or less) of the exhaust plume of a single ship to be 2 days. Increased concentrations of NO<sub>x</sub> (= NO + NO<sub>2</sub>) in the plume air lead to higher catalytical photochemical production rates of O<sub>3</sub> and also of OH. Due to increased OH concentrations in the plume, the lifetime of many species (especially NO<sub>x</sub>) is significantly reduced in plume air. The chemistry on background aerosols has a significant effect on gas phase chemistry in the ship plume, while partly soluble ship-produced aerosols are computed to only have a very small effect. Soot particles emitted by ships showed no effect on gas phase chemistry. Halogen species that are released from sea salt aerosols are slightly increased in plume air. In the early plume stages, however, the mixing ratio of BrO is decreased because it reacts rapidly with NO. To study the global effects of ship emissions we used a simple upscaling approach which suggested that the parameterization of ship emissions in global chemistry models as a constant source at the sea surface leads to an overestimation of the effects of ship emissions on O<sub>3</sub> of about 50% and on OH of roughly a factor of 2. The differences are mainly caused by a strongly reduced lifetime (compared to background air) of NO<sub>x</sub>in the early stages of a ship plume.http://www.atmos-chem-phys.net/3/233/2003/acp-3-233-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author R. von Glasow
R. von Glasow
M. G. Lawrence
R. Sander
P. J. Crutzen
P. J. Crutzen
spellingShingle R. von Glasow
R. von Glasow
M. G. Lawrence
R. Sander
P. J. Crutzen
P. J. Crutzen
Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
Atmospheric Chemistry and Physics
author_facet R. von Glasow
R. von Glasow
M. G. Lawrence
R. Sander
P. J. Crutzen
P. J. Crutzen
author_sort R. von Glasow
title Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
title_short Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
title_full Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
title_fullStr Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
title_full_unstemmed Modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
title_sort modeling the chemical effects of ship exhaust in the cloud-free marine boundary layer
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2003-01-01
description The chemical evolution of the exhaust plumes of ocean-going ships in the cloud-free marine boundary layer is examined with a box model. Dilution of the ship plume via entrainment of background air was treated as in studies of aircraft emissions and was found to be a very important process that significantly alters model results. We estimated the chemical lifetime (defined as the time when differences between plume and background air are reduced to 5% or less) of the exhaust plume of a single ship to be 2 days. Increased concentrations of NO<sub>x</sub> (= NO + NO<sub>2</sub>) in the plume air lead to higher catalytical photochemical production rates of O<sub>3</sub> and also of OH. Due to increased OH concentrations in the plume, the lifetime of many species (especially NO<sub>x</sub>) is significantly reduced in plume air. The chemistry on background aerosols has a significant effect on gas phase chemistry in the ship plume, while partly soluble ship-produced aerosols are computed to only have a very small effect. Soot particles emitted by ships showed no effect on gas phase chemistry. Halogen species that are released from sea salt aerosols are slightly increased in plume air. In the early plume stages, however, the mixing ratio of BrO is decreased because it reacts rapidly with NO. To study the global effects of ship emissions we used a simple upscaling approach which suggested that the parameterization of ship emissions in global chemistry models as a constant source at the sea surface leads to an overestimation of the effects of ship emissions on O<sub>3</sub> of about 50% and on OH of roughly a factor of 2. The differences are mainly caused by a strongly reduced lifetime (compared to background air) of NO<sub>x</sub>in the early stages of a ship plume.
url http://www.atmos-chem-phys.net/3/233/2003/acp-3-233-2003.pdf
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