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

Producción científica: Conference contribution

Resumen

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 de la publicación alojada	Norwegian Ocean Climate Project
Subtítulo de la publicación alojada	Technical Report No. 3
Editorial	University of Berlin
Páginas	35-40
Número de páginas	6
Edición	No. 3
Estado	Published - 2002
Evento	NOClim Science meeting 2002 - Clarion Hotel Oslo Airport, Gardermoen, Norway Duración: 13 may 2002 → 15 may 2002 https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf

Serie de la publicación

Nombre	Norwegian Ocean Climate Project. Technical Report
Editorial	University of Bergen

Conference

Conference	NOClim Science meeting 2002
País/Territorio	Norway
Ciudad	Gardermoen
Período	13/05/02 → 15/05/02
Dirección de internet	https://folk.uib.no/ngfls/NOClimI/Documents/TecRep3.pdf

Acceder al documento

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

Citar esto

@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 ). En Norwegian Ocean Climate Project : Technical Report No. 3 . No. 3 ed., 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 )

Resumen

Serie de la publicación

Conference

Acceder al documento

Huella

Citar esto