A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )

Peter Wadhams; Edmond Hanson; Jeremy Wilkinson

A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )

Peter Wadhams
, Edmond Hanson
, Jeremy Wilkinson

SAMS UHI

Resultado de pesquisa: Conference contribution

Resumo

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.

Idioma original	English
Título da publicação do anfitrião	Norwegian Ocean Climate Project
Subtítulo da publicação do anfitrião	Technical Report No. 3
Editora	University of Berlin
Páginas	35-40
Número de páginas	6
Edição	No. 3
Estado da publicação	Published - 2002
Evento	NOClim Science meeting 2002 - Clarion Hotel Oslo Airport, Gardermoen, Norway Duração: 13 mai. 2002 → 15 mai. 2002 https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf

Série de publicação

Nome	Norwegian Ocean Climate Project. Technical Report
Editora	University of Bergen

Conference

Conference	NOClim Science meeting 2002
País/Território	Norway
Cidade	Gardermoen
Período	13/05/02 → 15/05/02
Endereço da Internet	https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf

Acesso ao documento

https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf

Citar isto

@inproceedings{84471e5f9fe74021805213e8526288de,

title = "A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )",

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. ",

author = "Peter Wadhams and Edmond Hanson and Jeremy Wilkinson",

note = "Description - Edited by Solfrid S{\ae}tre Hj{\o}llo A shortened version, without figures, of a paper in press with Geophysical Research Letters) ; NOClim Science meeting 2002 ; Conference date: 13-05-2002 Through 15-05-2002",

year = "2002",

language = "English",

series = "Norwegian Ocean Climate Project. Technical Report",

publisher = "University of Berlin",

pages = "35--40",

booktitle = "Norwegian Ocean Climate Project",

address = "Germany",

edition = "No. 3",

url = "https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf",

}

Wadhams, P, Hanson, E & Wilkinson, J 2002, A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson ). em Norwegian Ocean Climate Project : Technical Report No. 3 . No. 3 edn, Norwegian Ocean Climate Project. Technical Report, University of Berlin, pp. 35-40, NOClim Science meeting 2002 , Gardermoen, Norway, 13/05/02. <https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf>

TY - GEN

T1 - A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )

AU - Wadhams, Peter

AU - Hanson, Edmond

AU - Wilkinson, Jeremy

N1 - Description - Edited by Solfrid Sætre Hjøllo A shortened version, without figures, of a paper in press with Geophysical Research Letters)

PY - 2002

Y1 - 2002

N2 - 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.

AB - 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.

M3 - Conference contribution

T3 - Norwegian Ocean Climate Project. Technical Report

SP - 35

EP - 40

BT - Norwegian Ocean Climate Project

PB - University of Berlin

T2 - NOClim Science meeting 2002

Y2 - 13 May 2002 through 15 May 2002

ER -

A Deep Convective Chimney in the Winter Greenland Sea (Wadhams, Hansen and Wilkinson )

Resumo

Série de publicação

Conference

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