Rapid coupling between ice volume and polar temperature over the past 150,000 years
Rapid coupling between ice volume and polar temperature over the past 150,000 years
Current global warming necessitates a detailed understanding of the relationships between climate and global ice volume. Highly resolved and continuous sea-level records are essential for quantifying ice-volume changes. However, an unbiased study of the timing of past ice-volume changes, relative to polar climate change, has so far been impossible because available sea-level records either were dated by using orbital tuning or ice-core timescales, or were discontinuous in time. Here we present an independent dating of a continuous, high-resolution sea-level record1, 2 in millennial-scale detail throughout the past 150,000 years. We find that the timing of ice-volume fluctuations agrees well with that of variations in Antarctic climate and especially Greenland climate. Amplitudes of ice-volume fluctuations more closely match Antarctic (rather than Greenland) climate changes. Polar climate and ice-volume changes, and their rates of change, are found to covary within centennial response times. Finally, rates of sea-level rise reached at least 1.2?m per century during all major episodes of ice-volume reduction.
744-747
Grant, K.M.
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Rohling, E.J.
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Bar-Matthews, M.
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Ayalon, A.
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Medina-Elizalde, M.
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Ramsey, C. Bronk
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Satow, C.
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Roberts, A.P.
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29 November 2012
Grant, K.M.
f9d9fa1b-62f3-4e90-a6f0-b46bc213fdb2
Rohling, E.J.
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Bar-Matthews, M.
cd213b3b-13c3-4bd3-ac5d-a2deebba523a
Ayalon, A.
38e49527-cfa0-44e7-be53-d2df2e0a3cf6
Medina-Elizalde, M.
e3c33ced-06eb-463b-9835-1f6397213c2f
Ramsey, C. Bronk
bc349746-629c-4d06-8ffb-6399877c9a94
Satow, C.
799af4ba-40e3-46a4-9c99-f54697fb3a80
Roberts, A.P.
4497b436-ef02-428d-a46e-65a22094ba52
Grant, K.M., Rohling, E.J., Bar-Matthews, M., Ayalon, A., Medina-Elizalde, M., Ramsey, C. Bronk, Satow, C. and Roberts, A.P.
(2012)
Rapid coupling between ice volume and polar temperature over the past 150,000 years.
Nature, 491, .
(doi:10.1038/nature11593).
Abstract
Current global warming necessitates a detailed understanding of the relationships between climate and global ice volume. Highly resolved and continuous sea-level records are essential for quantifying ice-volume changes. However, an unbiased study of the timing of past ice-volume changes, relative to polar climate change, has so far been impossible because available sea-level records either were dated by using orbital tuning or ice-core timescales, or were discontinuous in time. Here we present an independent dating of a continuous, high-resolution sea-level record1, 2 in millennial-scale detail throughout the past 150,000 years. We find that the timing of ice-volume fluctuations agrees well with that of variations in Antarctic climate and especially Greenland climate. Amplitudes of ice-volume fluctuations more closely match Antarctic (rather than Greenland) climate changes. Polar climate and ice-volume changes, and their rates of change, are found to covary within centennial response times. Finally, rates of sea-level rise reached at least 1.2?m per century during all major episodes of ice-volume reduction.
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e-pub ahead of print date: 2012
Published date: 29 November 2012
Organisations:
Paleooceanography & Palaeoclimate
Identifiers
Local EPrints ID: 345297
URI: http://eprints.soton.ac.uk/id/eprint/345297
ISSN: 0028-0836
PURE UUID: 9bd3c9aa-5fad-4b07-a929-6552db2bf6fb
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Date deposited: 16 Nov 2012 09:26
Last modified: 15 Mar 2024 02:47
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Contributors
Author:
K.M. Grant
Author:
M. Bar-Matthews
Author:
A. Ayalon
Author:
M. Medina-Elizalde
Author:
C. Bronk Ramsey
Author:
C. Satow
Author:
A.P. Roberts
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