Potential sea salt aerosol sources from frost flowers in the pan-Arctic region
In order to better represent observed wintertime aerosol concentrations at Barrow, Alaska, we implemented an observationally-based parameterization for estimating sea salt production from frost flowers in the Community Earth System Model (CESM). In this work, we evaluate the potential influence of t...
Published in: | Journal of Geophysical Research: Atmospheres |
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Online Access: | http://www.osti.gov/servlets/purl/1340876 https://www.osti.gov/biblio/1340876 https://doi.org/10.1002/2015JD024713 |
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ftosti:oai:osti.gov:1340876 2023-07-30T04:01:14+02:00 Potential sea salt aerosol sources from frost flowers in the pan-Arctic region Xu, Li Russell, Lynn M. Burrows, Susannah M. 2022-05-23 application/pdf http://www.osti.gov/servlets/purl/1340876 https://www.osti.gov/biblio/1340876 https://doi.org/10.1002/2015JD024713 unknown http://www.osti.gov/servlets/purl/1340876 https://www.osti.gov/biblio/1340876 https://doi.org/10.1002/2015JD024713 doi:10.1002/2015JD024713 54 ENVIRONMENTAL SCIENCES 2022 ftosti https://doi.org/10.1002/2015JD024713 2023-07-11T09:16:56Z In order to better represent observed wintertime aerosol concentrations at Barrow, Alaska, we implemented an observationally-based parameterization for estimating sea salt production from frost flowers in the Community Earth System Model (CESM). In this work, we evaluate the potential influence of this sea salt source on the pan-Arctic (60ºN-90ºN) climate. Results show that frost flower salt emissions substantially increase the modeled surface sea salt aerosol concentration in the winter months when new sea ice and frost flowers are present. The parameterization reproduces both the magnitude and seasonal variation of the observed submicron sea salt aerosol concentration at surface in Barrow during winter much better than the standard CESM simulation without a frost-flower salt particle source. Adding these frost flower salt particle emissions increases aerosol optical depth by 10% and results in a small cooling at surface. Here, the increase in salt particle mass concentrations of a factor of 8 provides nearly two times the cloud condensation nuclei concentration, as well as 10% increases in cloud droplet number and 40% increases in liquid water content near coastal regions adjacent to continents. These cloud changes reduce longwave cloud forcing by 3% and cause a small surface warming, increasing the downward longwave flux at the surface by 2 W m -2 in the pan-Arctic under the present-day climate. Other/Unknown Material Arctic Barrow Sea ice Alaska SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) Arctic Journal of Geophysical Research: Atmospheres 121 18 10,840 10,856 |
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Open Polar |
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SciTec Connect (Office of Scientific and Technical Information - OSTI, U.S. Department of Energy) |
op_collection_id |
ftosti |
language |
unknown |
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54 ENVIRONMENTAL SCIENCES |
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54 ENVIRONMENTAL SCIENCES Xu, Li Russell, Lynn M. Burrows, Susannah M. Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
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54 ENVIRONMENTAL SCIENCES |
description |
In order to better represent observed wintertime aerosol concentrations at Barrow, Alaska, we implemented an observationally-based parameterization for estimating sea salt production from frost flowers in the Community Earth System Model (CESM). In this work, we evaluate the potential influence of this sea salt source on the pan-Arctic (60ºN-90ºN) climate. Results show that frost flower salt emissions substantially increase the modeled surface sea salt aerosol concentration in the winter months when new sea ice and frost flowers are present. The parameterization reproduces both the magnitude and seasonal variation of the observed submicron sea salt aerosol concentration at surface in Barrow during winter much better than the standard CESM simulation without a frost-flower salt particle source. Adding these frost flower salt particle emissions increases aerosol optical depth by 10% and results in a small cooling at surface. Here, the increase in salt particle mass concentrations of a factor of 8 provides nearly two times the cloud condensation nuclei concentration, as well as 10% increases in cloud droplet number and 40% increases in liquid water content near coastal regions adjacent to continents. These cloud changes reduce longwave cloud forcing by 3% and cause a small surface warming, increasing the downward longwave flux at the surface by 2 W m -2 in the pan-Arctic under the present-day climate. |
author |
Xu, Li Russell, Lynn M. Burrows, Susannah M. |
author_facet |
Xu, Li Russell, Lynn M. Burrows, Susannah M. |
author_sort |
Xu, Li |
title |
Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
title_short |
Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
title_full |
Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
title_fullStr |
Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
title_full_unstemmed |
Potential sea salt aerosol sources from frost flowers in the pan-Arctic region |
title_sort |
potential sea salt aerosol sources from frost flowers in the pan-arctic region |
publishDate |
2022 |
url |
http://www.osti.gov/servlets/purl/1340876 https://www.osti.gov/biblio/1340876 https://doi.org/10.1002/2015JD024713 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Barrow Sea ice Alaska |
genre_facet |
Arctic Barrow Sea ice Alaska |
op_relation |
http://www.osti.gov/servlets/purl/1340876 https://www.osti.gov/biblio/1340876 https://doi.org/10.1002/2015JD024713 doi:10.1002/2015JD024713 |
op_doi |
https://doi.org/10.1002/2015JD024713 |
container_title |
Journal of Geophysical Research: Atmospheres |
container_volume |
121 |
container_issue |
18 |
container_start_page |
10,840 |
op_container_end_page |
10,856 |
_version_ |
1772811986133843968 |