Abstract
During two cruises to the Greenland Sea in winter 2001 a narrow convective chimney extending from the surface to a depth exceeding 2400 meters was is covered and mapped in detail. The feature was observed to be stable over a period of a month and its centre moved only 700 m in that time; its diameter was only 10 km. At a time when deep convection is thought to have ceased in the Greenland Sea the existence of this feature is a challenge to our understanding of the causes and impacts of open ocean winter convection.
Original language | English |
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Title of host publication | Norwegian Ocean Climate Project |
Subtitle of host publication | Technical Report No. 3 |
Publisher | University of Berlin |
Pages | 35-40 |
Number of pages | 6 |
Edition | No. 3 |
Publication status | Published - 2002 |
Event | NOClim Science meeting 2002 - Clarion Hotel Oslo Airport, Gardermoen, Norway Duration: 13 May 2002 → 15 May 2002 https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf |
Publication series
Name | Norwegian Ocean Climate Project. Technical Report |
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Publisher | University of Bergen |
Conference
Conference | NOClim Science meeting 2002 |
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Country/Territory | Norway |
City | Gardermoen |
Period | 13/05/02 → 15/05/02 |
Internet address |