Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence
With the sea-ice decline over the eastern part of the Eurasian Arctic (EEA), polar mesocyclones (MCs) and their most intensive representatives-polar lows (PLs)-can occur over more open-water areas. Visible and infrared MODIS images, active and passive microwave spaceborne instruments, and ERA Interi...
Published in: | IEEE Geoscience and Remote Sensing Letters |
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ftarchimer:oai:archimer.ifremer.fr:46870 2023-05-15T14:37:42+02:00 Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence Zabolotskikh, Elizaveta V. Gurvich, Irina A. Chapron, Bertrand 2016-10 application/pdf https://archimer.ifremer.fr/doc/00358/46870/48388.pdf https://doi.org/10.1109/LGRS.2016.2593487 https://archimer.ifremer.fr/doc/00358/46870/ eng eng Ieee-inst Electrical Electronics Engineers Inc https://archimer.ifremer.fr/doc/00358/46870/48388.pdf doi:10.1109/LGRS.2016.2593487 https://archimer.ifremer.fr/doc/00358/46870/ 2016 IEEE info:eu-repo/semantics/openAccess restricted use Ieee Geoscience And Remote Sensing Letters (1545-598X) (Ieee-inst Electrical Electronics Engineers Inc), 2016-10 , Vol. 13 , N. 10 , P. 1492-1496 Arctic geoscience mesoscale cyclones text Publication info:eu-repo/semantics/article 2016 ftarchimer https://doi.org/10.1109/LGRS.2016.2593487 2021-09-23T20:28:58Z With the sea-ice decline over the eastern part of the Eurasian Arctic (EEA), polar mesocyclones (MCs) and their most intensive representatives-polar lows (PLs)-can occur over more open-water areas. Visible and infrared MODIS images, active and passive microwave spaceborne instruments, and ERA Interim reanalysis data are combined and used to analyze the synoptic situations and to infer the factors influencingMC appearance and evolution over the Kara Sea, the Laptev Sea, the East Siberian Sea, and the Chukchi Sea. In recent years, the Arctic more often loses its summer sea-ice cover, and PLs may more commonly emerge within open-water Eastern Arctic regions during fall and summer months. This conclusion is derived basing on the analysis of more than 150 MCs for August, September, October, and November months over the EEA for the period of 2003-2015. PL and MC distribution and characteristics necessitate to be studied with a multisensor approach since neither reanalysis data nor data from a single instrument can provide sufficient means for their confident detection and analysis. Article in Journal/Newspaper Arctic Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Arctic Chukchi Sea East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Kara Sea Laptev Sea IEEE Geoscience and Remote Sensing Letters 13 10 1492 1496 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
Arctic geoscience mesoscale cyclones |
spellingShingle |
Arctic geoscience mesoscale cyclones Zabolotskikh, Elizaveta V. Gurvich, Irina A. Chapron, Bertrand Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
topic_facet |
Arctic geoscience mesoscale cyclones |
description |
With the sea-ice decline over the eastern part of the Eurasian Arctic (EEA), polar mesocyclones (MCs) and their most intensive representatives-polar lows (PLs)-can occur over more open-water areas. Visible and infrared MODIS images, active and passive microwave spaceborne instruments, and ERA Interim reanalysis data are combined and used to analyze the synoptic situations and to infer the factors influencingMC appearance and evolution over the Kara Sea, the Laptev Sea, the East Siberian Sea, and the Chukchi Sea. In recent years, the Arctic more often loses its summer sea-ice cover, and PLs may more commonly emerge within open-water Eastern Arctic regions during fall and summer months. This conclusion is derived basing on the analysis of more than 150 MCs for August, September, October, and November months over the EEA for the period of 2003-2015. PL and MC distribution and characteristics necessitate to be studied with a multisensor approach since neither reanalysis data nor data from a single instrument can provide sufficient means for their confident detection and analysis. |
format |
Article in Journal/Newspaper |
author |
Zabolotskikh, Elizaveta V. Gurvich, Irina A. Chapron, Bertrand |
author_facet |
Zabolotskikh, Elizaveta V. Gurvich, Irina A. Chapron, Bertrand |
author_sort |
Zabolotskikh, Elizaveta V. |
title |
Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
title_short |
Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
title_full |
Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
title_fullStr |
Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
title_full_unstemmed |
Polar Lows Over the Eastern Part of the Eurasian Arctic: The Sea-Ice Retreat Consequence |
title_sort |
polar lows over the eastern part of the eurasian arctic: the sea-ice retreat consequence |
publisher |
Ieee-inst Electrical Electronics Engineers Inc |
publishDate |
2016 |
url |
https://archimer.ifremer.fr/doc/00358/46870/48388.pdf https://doi.org/10.1109/LGRS.2016.2593487 https://archimer.ifremer.fr/doc/00358/46870/ |
long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) |
geographic |
Arctic Chukchi Sea East Siberian Sea Kara Sea Laptev Sea |
geographic_facet |
Arctic Chukchi Sea East Siberian Sea Kara Sea Laptev Sea |
genre |
Arctic Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice |
genre_facet |
Arctic Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice |
op_source |
Ieee Geoscience And Remote Sensing Letters (1545-598X) (Ieee-inst Electrical Electronics Engineers Inc), 2016-10 , Vol. 13 , N. 10 , P. 1492-1496 |
op_relation |
https://archimer.ifremer.fr/doc/00358/46870/48388.pdf doi:10.1109/LGRS.2016.2593487 https://archimer.ifremer.fr/doc/00358/46870/ |
op_rights |
2016 IEEE info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.1109/LGRS.2016.2593487 |
container_title |
IEEE Geoscience and Remote Sensing Letters |
container_volume |
13 |
container_issue |
10 |
container_start_page |
1492 |
op_container_end_page |
1496 |
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1766309915947696128 |