Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic
Our lack of understanding with respect to the sources and nucleating capabilities of natural aerosol in the high Arctic is one reason why Arctic clouds are still poorly represented in climate models. Recent field campaigns provide evidence of a source of sea salt aerosol (SSA) from blowing snow abov...
Main Authors: | , , , , |
---|---|
Format: | Conference Object |
Language: | English |
Published: |
2023
|
Subjects: | |
Online Access: | https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018930 |
id |
ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018930 |
---|---|
record_format |
openpolar |
spelling |
ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018930 2023-10-01T03:53:29+02:00 Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic Kirchgaessner, A. Frey, M. van den Heuvel, F. Yang, X. Lachlan-Cope, T. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018930 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2952 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018930 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-2952 2023-09-03T23:42:28Z Our lack of understanding with respect to the sources and nucleating capabilities of natural aerosol in the high Arctic is one reason why Arctic clouds are still poorly represented in climate models. Recent field campaigns provide evidence of a source of sea salt aerosol (SSA) from blowing snow above sea ice, which can account for the SSA winter/spring maxima observed in the Polar Regions. This SSA has the potential to influence the regional climate through the indirect radiative effect, but the relative magnitude of its contribution to cloud forming particles, especially ice nucleating particles (INP), are still largely unknown. For this presentation we use online and offline measurements of airborne aerosol for its ice nucleating properties that were carried out in the Central Arctic during MOSAiC. We combine these with INP measurements from snow samples, observations of snow particle fluxes, and aerosol measurements from the comprehensive MOSAiC data set. Online observations of INP in spring show concentrations in the order of a few tens [particle m-3], that were often associated with high wind speeds. Initial offline analyses of snow samples from the sea ice taken during the same period indicate the presence of INPs. This is evidence that snow on sea ice represents a viable source of INPs, which may release these particles via blowing snow into the atmosphere. Conference Object Arctic Sea ice GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Arctic |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
Our lack of understanding with respect to the sources and nucleating capabilities of natural aerosol in the high Arctic is one reason why Arctic clouds are still poorly represented in climate models. Recent field campaigns provide evidence of a source of sea salt aerosol (SSA) from blowing snow above sea ice, which can account for the SSA winter/spring maxima observed in the Polar Regions. This SSA has the potential to influence the regional climate through the indirect radiative effect, but the relative magnitude of its contribution to cloud forming particles, especially ice nucleating particles (INP), are still largely unknown. For this presentation we use online and offline measurements of airborne aerosol for its ice nucleating properties that were carried out in the Central Arctic during MOSAiC. We combine these with INP measurements from snow samples, observations of snow particle fluxes, and aerosol measurements from the comprehensive MOSAiC data set. Online observations of INP in spring show concentrations in the order of a few tens [particle m-3], that were often associated with high wind speeds. Initial offline analyses of snow samples from the sea ice taken during the same period indicate the presence of INPs. This is evidence that snow on sea ice represents a viable source of INPs, which may release these particles via blowing snow into the atmosphere. |
format |
Conference Object |
author |
Kirchgaessner, A. Frey, M. van den Heuvel, F. Yang, X. Lachlan-Cope, T. |
spellingShingle |
Kirchgaessner, A. Frey, M. van den Heuvel, F. Yang, X. Lachlan-Cope, T. Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
author_facet |
Kirchgaessner, A. Frey, M. van den Heuvel, F. Yang, X. Lachlan-Cope, T. |
author_sort |
Kirchgaessner, A. |
title |
Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
title_short |
Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
title_full |
Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
title_fullStr |
Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
title_full_unstemmed |
Sea salt aerosol in snow on sea ice as a potential source of Ice Nucleating Particles in the Arctic |
title_sort |
sea salt aerosol in snow on sea ice as a potential source of ice nucleating particles in the arctic |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018930 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-2952 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018930 |
op_doi |
https://doi.org/10.57757/IUGG23-2952 |
_version_ |
1778520104980447232 |