Regional impacts of ultrafine particle emissions from the surface of the Great Lakes

Quantifying the impacts of aerosols on climate requires a detailed knowledge of both the anthropogenic and the natural contributions to the aerosol population. Recent work has suggested a previously unrecognized natural source of ultrafine particles resulting from breaking waves at the surface of la...

Full description

Bibliographic Details
Main Authors: S. H. Chung, B. M. Basarab, T. M. VanReken
Format: Article
Language:English
Published: Copernicus Publications 2011-12-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/11/12601/2011/acp-11-12601-2011.pdf
id doaj-11a1ba4b6b9142f1af46436b65ab1826
record_format Article
spelling doaj-11a1ba4b6b9142f1af46436b65ab18262020-11-24T23:15:47ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242011-12-011124126011261510.5194/acp-11-12601-2011Regional impacts of ultrafine particle emissions from the surface of the Great LakesS. H. ChungB. M. BasarabT. M. VanRekenQuantifying the impacts of aerosols on climate requires a detailed knowledge of both the anthropogenic and the natural contributions to the aerosol population. Recent work has suggested a previously unrecognized natural source of ultrafine particles resulting from breaking waves at the surface of large freshwater lakes. This work is the first modeling study to investigate the potential for this newly discovered source to affect the aerosol number concentrations on regional scales. Using the WRF-Chem modeling framework, the impacts of wind-driven aerosol production from the surface of the Great Lakes were studied for a July 2004 test case. Simulations were performed for a base case with no lake surface emissions, a case with lake surface emissions included, and a default case wherein large freshwater lakes emit marine particles as if they were oceans. Results indicate that the lake surface emissions can enhance the surface-level aerosol number concentration by ~20% over the remote northern Great Lakes and by ~5% over other parts of the Great Lakes. These results were highly sensitive to the new particle formation (i.e., nucleation) parameterization within WRF-Chem; when the new particle formation process was deactivated, surface-layer enhancements from the lake emissions increased to as much as 200%. The results reported here have significant uncertainties associated with the lake emission parameterization and the way ultrafine particles are modeled within WRF-Chem. Nevertheless, the magnitudes of the impacts found in this study suggest that further study to quantify the emissions of ultrafine particles from the surface of the Great Lakes is merited.http://www.atmos-chem-phys.net/11/12601/2011/acp-11-12601-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. H. Chung
B. M. Basarab
T. M. VanReken
spellingShingle S. H. Chung
B. M. Basarab
T. M. VanReken
Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
Atmospheric Chemistry and Physics
author_facet S. H. Chung
B. M. Basarab
T. M. VanReken
author_sort S. H. Chung
title Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
title_short Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
title_full Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
title_fullStr Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
title_full_unstemmed Regional impacts of ultrafine particle emissions from the surface of the Great Lakes
title_sort regional impacts of ultrafine particle emissions from the surface of the great lakes
publisher Copernicus Publications
series Atmospheric Chemistry and Physics
issn 1680-7316
1680-7324
publishDate 2011-12-01
description Quantifying the impacts of aerosols on climate requires a detailed knowledge of both the anthropogenic and the natural contributions to the aerosol population. Recent work has suggested a previously unrecognized natural source of ultrafine particles resulting from breaking waves at the surface of large freshwater lakes. This work is the first modeling study to investigate the potential for this newly discovered source to affect the aerosol number concentrations on regional scales. Using the WRF-Chem modeling framework, the impacts of wind-driven aerosol production from the surface of the Great Lakes were studied for a July 2004 test case. Simulations were performed for a base case with no lake surface emissions, a case with lake surface emissions included, and a default case wherein large freshwater lakes emit marine particles as if they were oceans. Results indicate that the lake surface emissions can enhance the surface-level aerosol number concentration by ~20% over the remote northern Great Lakes and by ~5% over other parts of the Great Lakes. These results were highly sensitive to the new particle formation (i.e., nucleation) parameterization within WRF-Chem; when the new particle formation process was deactivated, surface-layer enhancements from the lake emissions increased to as much as 200%. The results reported here have significant uncertainties associated with the lake emission parameterization and the way ultrafine particles are modeled within WRF-Chem. Nevertheless, the magnitudes of the impacts found in this study suggest that further study to quantify the emissions of ultrafine particles from the surface of the Great Lakes is merited.
url http://www.atmos-chem-phys.net/11/12601/2011/acp-11-12601-2011.pdf
work_keys_str_mv AT shchung regionalimpactsofultrafineparticleemissionsfromthesurfaceofthegreatlakes
AT bmbasarab regionalimpactsofultrafineparticleemissionsfromthesurfaceofthegreatlakes
AT tmvanreken regionalimpactsofultrafineparticleemissionsfromthesurfaceofthegreatlakes
_version_ 1725589519704522752