A change in seasonality in Greenland during a Dansgaard–Oeschger warming

A new sub-seasonal chemical record is presented from the North Greenland Icecore Project (NorthGRIP) ice core during the onset of one of the longest and strongest interstadials of the last glacial period, Dansgaard–Oeschger event 8 (approximately 38 000 years ago). This is the first time that a reco...

Full description

Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Thomas, Elizabeth R., Mulvaney, Robert, Wolff, Eric W.
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2008
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/3268/
https://nora.nerc.ac.uk/id/eprint/3268/1/Thomas_et_al.,_2008_annals_of_glaciology.pdf
https://doi.org/10.3189/172756408784700590
Description
Summary:A new sub-seasonal chemical record is presented from the North Greenland Icecore Project (NorthGRIP) ice core during the onset of one of the longest and strongest interstadials of the last glacial period, Dansgaard–Oeschger event 8 (approximately 38 000 years ago). This is the first time that a record of such resolution has been achieved over several metres of deep glacial ice and provides a unique opportunity for using additional parameters to carry out accurate dating using annual-layer counting. The very high-resolution chemical data were used to assess the phasing of various ions and determine changes in the seasonal strength of chemical deposition and the shape of the seasonal cycle. The study shows that a change in seasonality accompanied the dramatic warming transition from stadial to interstadial conditions in Greenland.