Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores

Decadal means of &delta;<sup>18</sup>O and accumulation rates from 52 ice core locations in Greenland are presented. The accumulation rates are derived from annual layers determined in the &delta;<sup>18</sup>O curve. Investigation of the &delta;<sup>18&l...

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Main Authors: D. Dahl-Jensen, B. M. Vinther, H. B. Clausen, S. L. Buchardt
Format: Article
Language:English
Published: Copernicus Publications 2012-12-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/8/2053/2012/cp-8-2053-2012.pdf
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spelling doaj-17c3405c1c554ababe658a1ee21bdb482020-11-25T01:43:56ZengCopernicus PublicationsClimate of the Past1814-93241814-93322012-12-01862053205910.5194/cp-8-2053-2012Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice coresD. Dahl-JensenB. M. VintherH. B. ClausenS. L. BuchardtDecadal means of &delta;<sup>18</sup>O and accumulation rates from 52 ice core locations in Greenland are presented. The accumulation rates are derived from annual layers determined in the &delta;<sup>18</sup>O curve. Investigation of the &delta;<sup>18</sup>O-accumulation relationship across the ice divide reveals a significant Foehn effect with anticorrelation of &delta;<sup>18</sup>O and accumulation rate on the lee side of the divide in Southern Greenland, while no effect is seen in Central Greenland. Furthermore, the sensitivity of accumulation rate to changes in temperature is found to be smaller in Northern Greenland than in the central and southern parts. Four records in the data set contain sufficient recent data that the period of observed temperature rise from the 1990s and onwards can be investigated. All four records are from locations close to the ice divide in Northern Greenland and while three of them show increased temperatures, no conclusive statement can be made about the accumulation rate from these data.http://www.clim-past.net/8/2053/2012/cp-8-2053-2012.pdf
collection DOAJ
language English
format Article
sources DOAJ
author D. Dahl-Jensen
B. M. Vinther
H. B. Clausen
S. L. Buchardt
spellingShingle D. Dahl-Jensen
B. M. Vinther
H. B. Clausen
S. L. Buchardt
Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
Climate of the Past
author_facet D. Dahl-Jensen
B. M. Vinther
H. B. Clausen
S. L. Buchardt
author_sort D. Dahl-Jensen
title Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
title_short Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
title_full Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
title_fullStr Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
title_full_unstemmed Investigating the past and recent &delta;<sup>18</sup>O-accumulation relationship seen in Greenland ice cores
title_sort investigating the past and recent &delta;<sup>18</sup>o-accumulation relationship seen in greenland ice cores
publisher Copernicus Publications
series Climate of the Past
issn 1814-9324
1814-9332
publishDate 2012-12-01
description Decadal means of &delta;<sup>18</sup>O and accumulation rates from 52 ice core locations in Greenland are presented. The accumulation rates are derived from annual layers determined in the &delta;<sup>18</sup>O curve. Investigation of the &delta;<sup>18</sup>O-accumulation relationship across the ice divide reveals a significant Foehn effect with anticorrelation of &delta;<sup>18</sup>O and accumulation rate on the lee side of the divide in Southern Greenland, while no effect is seen in Central Greenland. Furthermore, the sensitivity of accumulation rate to changes in temperature is found to be smaller in Northern Greenland than in the central and southern parts. Four records in the data set contain sufficient recent data that the period of observed temperature rise from the 1990s and onwards can be investigated. All four records are from locations close to the ice divide in Northern Greenland and while three of them show increased temperatures, no conclusive statement can be made about the accumulation rate from these data.
url http://www.clim-past.net/8/2053/2012/cp-8-2053-2012.pdf
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