Aerosols indirectly warm the Arctic
On average, airborne aerosol particles cool the Earth’s surface directly by absorbingand scattering sunlight and indirectly by influencing cloud reflectivity, life time, thicknessor extent. Here we show that over the central Arctic Ocean, where there is frequentlya lack of aerosol particles upon whi...
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ftethz:oai:www.research-collection.ethz.ch:20.500.11850/28541 2023-05-15T14:42:43+02:00 Aerosols indirectly warm the Arctic Mauritsen, Thorsten Sedlar, Joseph Tjernström, Michael Leck, Caroline Martin, M. Shupe, Matthew Sjogren, S. Sierau, Berko Persson, P.O.G. Brooks, Ian M. Swietlicki, Erik 2011 application/application/pdf https://hdl.handle.net/20.500.11850/28541 https://doi.org/10.3929/ethz-b-000028541 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/acpd-10-16775-2010 http://hdl.handle.net/20.500.11850/28541 doi:10.3929/ethz-b-000028541 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/3.0/ Creative Commons Attribution 3.0 Unported CC-BY Atmospheric Chemistry and Physics, 10 (7) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2011 ftethz https://doi.org/20.500.11850/28541 https://doi.org/10.3929/ethz-b-000028541 https://doi.org/10.5194/acpd-10-16775-2010 2023-02-13T00:48:44Z On average, airborne aerosol particles cool the Earth’s surface directly by absorbingand scattering sunlight and indirectly by influencing cloud reflectivity, life time, thicknessor extent. Here we show that over the central Arctic Ocean, where there is frequentlya lack of aerosol particles upon which clouds may form, a small increase in aerosol5loading may enhance cloudiness thereby likely causing a climatologically significantwarming at the ice-covered Arctic surface. Under these low concentration conditionscloud droplets grow to drizzle sizes and fall, even in the absence of collisions andcoalescence, thereby diminishing cloud water. Evidence from a case study suggeststhat interactions between aerosol, clouds and precipitation could be responsible for10attaining the observed low aerosol concentrations. ISSN:1680-7375 ISSN:1680-7367 Article in Journal/Newspaper Arctic Arctic Ocean ETH Zürich Research Collection Arctic Arctic Ocean |
institution |
Open Polar |
collection |
ETH Zürich Research Collection |
op_collection_id |
ftethz |
language |
English |
description |
On average, airborne aerosol particles cool the Earth’s surface directly by absorbingand scattering sunlight and indirectly by influencing cloud reflectivity, life time, thicknessor extent. Here we show that over the central Arctic Ocean, where there is frequentlya lack of aerosol particles upon which clouds may form, a small increase in aerosol5loading may enhance cloudiness thereby likely causing a climatologically significantwarming at the ice-covered Arctic surface. Under these low concentration conditionscloud droplets grow to drizzle sizes and fall, even in the absence of collisions andcoalescence, thereby diminishing cloud water. Evidence from a case study suggeststhat interactions between aerosol, clouds and precipitation could be responsible for10attaining the observed low aerosol concentrations. ISSN:1680-7375 ISSN:1680-7367 |
format |
Article in Journal/Newspaper |
author |
Mauritsen, Thorsten Sedlar, Joseph Tjernström, Michael Leck, Caroline Martin, M. Shupe, Matthew Sjogren, S. Sierau, Berko Persson, P.O.G. Brooks, Ian M. Swietlicki, Erik |
spellingShingle |
Mauritsen, Thorsten Sedlar, Joseph Tjernström, Michael Leck, Caroline Martin, M. Shupe, Matthew Sjogren, S. Sierau, Berko Persson, P.O.G. Brooks, Ian M. Swietlicki, Erik Aerosols indirectly warm the Arctic |
author_facet |
Mauritsen, Thorsten Sedlar, Joseph Tjernström, Michael Leck, Caroline Martin, M. Shupe, Matthew Sjogren, S. Sierau, Berko Persson, P.O.G. Brooks, Ian M. Swietlicki, Erik |
author_sort |
Mauritsen, Thorsten |
title |
Aerosols indirectly warm the Arctic |
title_short |
Aerosols indirectly warm the Arctic |
title_full |
Aerosols indirectly warm the Arctic |
title_fullStr |
Aerosols indirectly warm the Arctic |
title_full_unstemmed |
Aerosols indirectly warm the Arctic |
title_sort |
aerosols indirectly warm the arctic |
publisher |
Copernicus |
publishDate |
2011 |
url |
https://hdl.handle.net/20.500.11850/28541 https://doi.org/10.3929/ethz-b-000028541 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_source |
Atmospheric Chemistry and Physics, 10 (7) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.5194/acpd-10-16775-2010 http://hdl.handle.net/20.500.11850/28541 doi:10.3929/ethz-b-000028541 |
op_rights |
info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/3.0/ Creative Commons Attribution 3.0 Unported |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/20.500.11850/28541 https://doi.org/10.3929/ethz-b-000028541 https://doi.org/10.5194/acpd-10-16775-2010 |
_version_ |
1766314449495392256 |