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Consistently dated records from the Greenland GRIP, GISP2 and NGRIP ice cores for the past 104 ka reveal regional millennial-scale δ18O gradients with possible Heinrich event imprint

Inger K. Seierstad, Peter Abbott Orcid Logo, Matthias Bigler, Thomas Blunier, Anna Bourne Orcid Logo, Edward Brook, Susanne L. Buchardt, Christo Buizert, Henrik B. Clausen, Eliza Cook, Dorthe Dahl-Jensen, Siwan Davies Orcid Logo, Myriam Guillevic, Sigfús J. Johnsen, Desirée S. Pedersen, Trevor J. Popp, Sune O. Rasmussen, Jeffrey P. Severinghaus, Anders Svensson, Bo M. Vinther

Quaternary Science Reviews, Volume: 106, Pages: 29 - 46

Swansea University Authors: Peter Abbott Orcid Logo, Anna Bourne Orcid Logo, Siwan Davies Orcid Logo

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Published in: Quaternary Science Reviews
ISSN: 0277-3791
Published: Elsevier BV 2014
Online Access: Check full text

URI: https://cronfa.swan.ac.uk/Record/cronfa19598
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Keywords: Paleoclimate; Greenland ice cores; GICC05 chronology; Tephra isochrons; Regional climate; Water isotopes (δ18O); Heinrich event
College: College of Science
Start Page: 29
End Page: 46