Cyclone impact on sea ice in the central Arctic Ocean: a statistical study
This study investigates the impact of cyclones on the Arctic Ocean sea ice for the first time in a statistical manner. We apply the coupled ice–ocean model NAOSIM which is forced by the ECMWF analyses for the period 2006–2008. Cyclone position and radius detected in the ECMWF data are used to extrac...
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ftdoajarticles:oai:doaj.org/article:ab9b828a67134077acdaf6b1d3510091 2023-05-15T13:11:02+02:00 Cyclone impact on sea ice in the central Arctic Ocean: a statistical study A. Kriegsmann B. Brümmer 2014-02-01T00:00:00Z https://doi.org/10.5194/tc-8-303-2014 https://doaj.org/article/ab9b828a67134077acdaf6b1d3510091 EN eng Copernicus Publications http://www.the-cryosphere.net/8/303/2014/tc-8-303-2014.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 1994-0416 1994-0424 doi:10.5194/tc-8-303-2014 https://doaj.org/article/ab9b828a67134077acdaf6b1d3510091 The Cryosphere, Vol 8, Iss 1, Pp 303-317 (2014) Environmental sciences GE1-350 Geology QE1-996.5 article 2014 ftdoajarticles https://doi.org/10.5194/tc-8-303-2014 2022-12-31T14:48:49Z This study investigates the impact of cyclones on the Arctic Ocean sea ice for the first time in a statistical manner. We apply the coupled ice–ocean model NAOSIM which is forced by the ECMWF analyses for the period 2006–2008. Cyclone position and radius detected in the ECMWF data are used to extract fields of wind, ice drift, and concentration from the ice–ocean model. Composite fields around the cyclone centre are calculated for different cyclone intensities, the four seasons, and different sub-regions of the Arctic Ocean. In total about 3500 cyclone events are analyzed. In general, cyclones reduce the ice concentration in the order of a few percent increasing towards the cyclone centre. This is confirmed by independent AMSR-E satellite data. The reduction increases with cyclone intensity and is most pronounced in summer and on the Siberian side of the Arctic Ocean. For the Arctic ice cover the cumulative impact of cyclones has climatologic consequences. In winter, the cyclone-induced openings refreeze so that the ice mass is increased. In summer, the openings remain open and the ice melt is accelerated via the positive albedo feedback. Strong summer storms on the Siberian side of the Arctic Ocean may have been important contributions to the recent ice extent minima in 2007 and 2012. Article in Journal/Newspaper albedo Arctic Arctic Ocean Sea ice The Cryosphere Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean The Cryosphere 8 1 303 317 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Environmental sciences GE1-350 Geology QE1-996.5 |
spellingShingle |
Environmental sciences GE1-350 Geology QE1-996.5 A. Kriegsmann B. Brümmer Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
topic_facet |
Environmental sciences GE1-350 Geology QE1-996.5 |
description |
This study investigates the impact of cyclones on the Arctic Ocean sea ice for the first time in a statistical manner. We apply the coupled ice–ocean model NAOSIM which is forced by the ECMWF analyses for the period 2006–2008. Cyclone position and radius detected in the ECMWF data are used to extract fields of wind, ice drift, and concentration from the ice–ocean model. Composite fields around the cyclone centre are calculated for different cyclone intensities, the four seasons, and different sub-regions of the Arctic Ocean. In total about 3500 cyclone events are analyzed. In general, cyclones reduce the ice concentration in the order of a few percent increasing towards the cyclone centre. This is confirmed by independent AMSR-E satellite data. The reduction increases with cyclone intensity and is most pronounced in summer and on the Siberian side of the Arctic Ocean. For the Arctic ice cover the cumulative impact of cyclones has climatologic consequences. In winter, the cyclone-induced openings refreeze so that the ice mass is increased. In summer, the openings remain open and the ice melt is accelerated via the positive albedo feedback. Strong summer storms on the Siberian side of the Arctic Ocean may have been important contributions to the recent ice extent minima in 2007 and 2012. |
format |
Article in Journal/Newspaper |
author |
A. Kriegsmann B. Brümmer |
author_facet |
A. Kriegsmann B. Brümmer |
author_sort |
A. Kriegsmann |
title |
Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
title_short |
Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
title_full |
Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
title_fullStr |
Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
title_full_unstemmed |
Cyclone impact on sea ice in the central Arctic Ocean: a statistical study |
title_sort |
cyclone impact on sea ice in the central arctic ocean: a statistical study |
publisher |
Copernicus Publications |
publishDate |
2014 |
url |
https://doi.org/10.5194/tc-8-303-2014 https://doaj.org/article/ab9b828a67134077acdaf6b1d3510091 |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
albedo Arctic Arctic Ocean Sea ice The Cryosphere |
genre_facet |
albedo Arctic Arctic Ocean Sea ice The Cryosphere |
op_source |
The Cryosphere, Vol 8, Iss 1, Pp 303-317 (2014) |
op_relation |
http://www.the-cryosphere.net/8/303/2014/tc-8-303-2014.pdf https://doaj.org/toc/1994-0416 https://doaj.org/toc/1994-0424 1994-0416 1994-0424 doi:10.5194/tc-8-303-2014 https://doaj.org/article/ab9b828a67134077acdaf6b1d3510091 |
op_doi |
https://doi.org/10.5194/tc-8-303-2014 |
container_title |
The Cryosphere |
container_volume |
8 |
container_issue |
1 |
container_start_page |
303 |
op_container_end_page |
317 |
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1766245690127679488 |