_version_ 1867169052256894976
author Steffensen, Jørgen Peder
Andersen, Katrine K
Bigler, Matthias
Clausen, Henrik Brink
Dahl-Jensen, Dorthe
Fischer, Hubertus
Goto-Azuma, Kumiko
Hansson, Margareta E
Johnsen, Sigfús Jóhann
Jouzel, Jean
Masson-Delmotte, Valerie
Popp, Trevor
Rasmussen, Sune Olander
Röthlisberger, Regine
Ruth, Urs
Stauffer, Bernhard
Siggaard-Andersen, Marie-Louise
Sveinbjörnsdottir, Árný E
Svensson, Anders M
White, James W C
author_facet Steffensen, Jørgen Peder
Andersen, Katrine K
Bigler, Matthias
Clausen, Henrik Brink
Dahl-Jensen, Dorthe
Fischer, Hubertus
Goto-Azuma, Kumiko
Hansson, Margareta E
Johnsen, Sigfús Jóhann
Jouzel, Jean
Masson-Delmotte, Valerie
Popp, Trevor
Rasmussen, Sune Olander
Röthlisberger, Regine
Ruth, Urs
Stauffer, Bernhard
Siggaard-Andersen, Marie-Louise
Sveinbjörnsdottir, Árný E
Svensson, Anders M
White, James W C
collection Datos científicos de ciencias marinas y ambientales
contents The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as recorded by stable water isotopes. The onsets of both abrupt Greenland warmings were slightly preceded by decreasing Greenland dust deposition, reflecting the wetting of Asian deserts. A northern shift of the Intertropical Convergence Zone could be the trigger of these abrupt shifts of Northern Hemisphere atmospheric circulation, resulting in changes of 2 to 4 kelvin in Greenland moisture source temperature from one year to the next.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_786474
institution PANGAEA
language en
publishDate 2008
publisher PANGAEA
record_format pangaea
spellingShingle (Data D1) Annual climate proxy data from the NGRIP ice core, Greenland
Steffensen, Jørgen Peder
Andersen, Katrine K
Bigler, Matthias
Clausen, Henrik Brink
Dahl-Jensen, Dorthe
Fischer, Hubertus
Goto-Azuma, Kumiko
Hansson, Margareta E
Johnsen, Sigfús Jóhann
Jouzel, Jean
Masson-Delmotte, Valerie
Popp, Trevor
Rasmussen, Sune Olander
Röthlisberger, Regine
Ruth, Urs
Stauffer, Bernhard
Siggaard-Andersen, Marie-Louise
Sveinbjörnsdottir, Árný E
Svensson, Anders M
White, James W C
AGE; Age, error; Annual layer thickness; Deuterium excess; Dust particles; Greenland; ICEDRILL; Ice drill; International Polar Year (2007-2008); ipy; IPY; NGRIP; North Greenland Ice Core Project; NorthGRIP; Parameter; Sampling/drilling ice; δ18O, water
The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as recorded by stable water isotopes. The onsets of both abrupt Greenland warmings were slightly preceded by decreasing Greenland dust deposition, reflecting the wetting of Asian deserts. A northern shift of the Intertropical Convergence Zone could be the trigger of these abrupt shifts of Northern Hemisphere atmospheric circulation, resulting in changes of 2 to 4 kelvin in Greenland moisture source temperature from one year to the next.
title (Data D1) Annual climate proxy data from the NGRIP ice core, Greenland
topic AGE; Age, error; Annual layer thickness; Deuterium excess; Dust particles; Greenland; ICEDRILL; Ice drill; International Polar Year (2007-2008); ipy; IPY; NGRIP; North Greenland Ice Core Project; NorthGRIP; Parameter; Sampling/drilling ice; δ18O, water
url https://doi.org/10.1594/PANGAEA.786474