Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)

Pierre Burckel; C. Waelbroeck; Y. Luo; D.M.V.A.P. Roche; S. Pichat; S. Jaccard; Jeanne Gherardi; A. Govin; Jorg Lippold; Francois Thil

doi:10.5194/cp-12-2061-2016

Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)

Pierre Burckel, C. Waelbroeck, Y. Luo, D.M.V.A.P. Roche, S. Pichat, S. Jaccard, Jeanne Gherardi, A. Govin, Jorg Lippold, Francois Thil

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

Original language	English
Pages (from-to)	2061-2075
Number of pages	15
Journal	Climate of the Past
Volume	12
DOIs	https://doi.org/10.5194/cp-12-2061-2016
Publication status	Published - 2016

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10.5194/cp-12-2061-2016

https://www.clim-past.net/12/2061/2016/Licence: CC BY-SA

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title = "Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)",

author = "Pierre Burckel and C. Waelbroeck and Y. Luo and D.M.V.A.P. Roche and S. Pichat and S. Jaccard and Jeanne Gherardi and A. Govin and Jorg Lippold and Francois Thil",

year = "2016",

doi = "10.5194/cp-12-2061-2016",

language = "English",

volume = "12",

pages = "2061--2075",

journal = "Climate of the Past",

issn = "1814-9324",

publisher = "Copernicus Publications",

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TY - JOUR

T1 - Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)

AU - Burckel, Pierre

AU - Waelbroeck, C.

AU - Luo, Y.

AU - Roche, D.M.V.A.P.

AU - Pichat, S.

AU - Jaccard, S.

AU - Gherardi, Jeanne

AU - Govin, A.

AU - Lippold, Jorg

AU - Thil, Francois

PY - 2016

Y1 - 2016

U2 - 10.5194/cp-12-2061-2016

DO - 10.5194/cp-12-2061-2016

M3 - Article

SN - 1814-9324

VL - 12

SP - 2061

EP - 2075

JO - Climate of the Past

JF - Climate of the Past

ER -

Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)

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Changes in the geometry and strength of the Atlantic meridional overturning circulation during the last glacial (20–50 ka)