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dc.contributor.authorQing Qin
dc.contributor.authorZhaomin Wang
dc.contributor.authorChengyan Liu
dc.contributor.authorChen Cheng
dc.date.accessioned2023-04-12T18:52:48Z
dc.date.available2023-04-12T18:52:48Z
dc.date.copyright2022/07/01
dc.date.issued2022
dc.identifier.otherJPO-D-21-0197.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4290406
dc.description.abstractExtensive studies have addressed the characteristics and mechanisms of open-ocean polynyas in the Weddell and Cosmonaut Seas. Here, we show that more persistent open-ocean polynyas occur in the Cooperation Sea (CS) (60°–90°E), a sector of the Southern Ocean off the Prydz Bay continental shelf, between 2002 and 2019. Polynyas are formed annually mainly within the 62°–65°S band, as identified by sea ice concentrations less than 0.7. The polynyas usually began to emerge in April and expanded to large sizes during July–October, with sizes often larger than those of the Maud Rise polynya in 2017. The annual maximum size of polynyas ranged from 115.3 × 10
dc.publisherAmerican Meteorological Society
dc.titleOpen-Ocean Polynyas in the Cooperation Sea, Antarctica
dc.typeJournal Paper
dc.journal.volume52
dc.journal.issue7
dc.journal.titleJournal of Physical Oceanography
dc.identifier.doi10.1175/JPO-D-21-0197.1
dc.journal.fristpage1363
dc.journal.lastpage1381
dc.page1363–1381
dc.treeJournal of Physical Oceanography:;2022:;volume( 052 ):;issue: 007
dc.contenttypeFulltext


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