Measured and smoothed sortable silt record of sediment core GS06-144-09MC-D

Changes in the Atlantic Meridional Overturning Circulation (AMOC) have commonly been invoked to explain the low‐frequency climate changes evident over millennial‐multidecadal timescales during the Holocene period. While there is growing evidence that deep ocean circulation varied on millennial times...

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Bibliographic Details
Main Authors: Mjell, Tor Lien, Ninnemann, Ulysses S, Kleiven, Helga F, Hall, Ian R
Format: Dataset
Language:English
Published: PANGAEA 2019
Subjects:
Age
AMV
MUC
NAO
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.899459
https://doi.org/10.1594/PANGAEA.899459