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 |
|---|---|
| Publisher | University of Bergen |
Conference
| Conference | NOClim Science meeting 2002 |
|---|---|
| Country/Territory | Norway |
| City | Gardermoen |
| Period | 13/05/02 → 15/05/02 |
| Internet address |