High-resolution Greenland Ice Core data show abrupt climate change happens in few years

Research output: Contribution to journal › Journal article › Research › peer-review

Standard

High-resolution Greenland Ice Core data show abrupt climate change happens in few years. / Steffensen, Jørgen Peder; Andersen, Katrine Krogh; Bigler, Matthias; Clausen, Henrik Brink; Dahl-Jensen, Dorthe; Fischer, Hubertus; Goto-Azuma, Kumiko; Hansson, Margareta; Johnsen, Sigfus Johann; Jouzel, Jean; Masson-Delmotte, Valérie; Popp, Trevor James; Rasmussen, Sune Olander; Röthlisberger, Regine; Ruth, Urs; Stauffer, Bernhard; Siggaard-Andersen, Marie-Louise; Sveinbjörnsdóttir, Árný E.; Svensson, Anders; White, James W.C.

In: Science, Vol. 321, 2008, p. 680-684.

Research output: Contribution to journal › Journal article › Research › peer-review

Harvard

Steffensen, JP, Andersen, KK, Bigler, M, Clausen, HB, Dahl-Jensen, D, Fischer, H, Goto-Azuma, K, Hansson, M, Johnsen, SJ, Jouzel, J, Masson-Delmotte, V, Popp, TJ, Rasmussen, SO, Röthlisberger, R, Ruth, U, Stauffer, B, Siggaard-Andersen, M-L, Sveinbjörnsdóttir, ÁE, Svensson, A & White, JWC 2008, 'High-resolution Greenland Ice Core data show abrupt climate change happens in few years', Science, vol. 321, pp. 680-684. https://doi.org/10.1126/science.1157707

APA

Steffensen, J. P., Andersen, K. K., Bigler, M., Clausen, H. B., Dahl-Jensen, D., Fischer, H., Goto-Azuma, K., Hansson, M., Johnsen, S. J., Jouzel, J., Masson-Delmotte, V., Popp, T. J., Rasmussen, S. O., Röthlisberger, R., Ruth, U., Stauffer, B., Siggaard-Andersen, M-L., Sveinbjörnsdóttir, Á. E., Svensson, A., & White, J. W. C. (2008). High-resolution Greenland Ice Core data show abrupt climate change happens in few years. Science, 321, 680-684. https://doi.org/10.1126/science.1157707

Vancouver

Steffensen JP, Andersen KK, Bigler M, Clausen HB, Dahl-Jensen D, Fischer H et al. High-resolution Greenland Ice Core data show abrupt climate change happens in few years. Science. 2008;321:680-684. https://doi.org/10.1126/science.1157707

Author

Steffensen, Jørgen Peder ; Andersen, Katrine Krogh ; Bigler, Matthias ; Clausen, Henrik Brink ; Dahl-Jensen, Dorthe ; Fischer, Hubertus ; Goto-Azuma, Kumiko ; Hansson, Margareta ; Johnsen, Sigfus Johann ; Jouzel, Jean ; Masson-Delmotte, Valérie ; Popp, Trevor James ; Rasmussen, Sune Olander ; Röthlisberger, Regine ; Ruth, Urs ; Stauffer, Bernhard ; Siggaard-Andersen, Marie-Louise ; Sveinbjörnsdóttir, Árný E. ; Svensson, Anders ; White, James W.C. / High-resolution Greenland Ice Core data show abrupt climate change happens in few years. In: Science. 2008 ; Vol. 321. pp. 680-684.

Bibtex

@article{c10ad3a0627911dd8d9f000ea68e967b,
title = "High-resolution Greenland Ice Core data show abrupt climate change happens in few years",
abstract = "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.",
author = "Steffensen, {J{\o}rgen Peder} and Andersen, {Katrine Krogh} and Matthias Bigler and Clausen, {Henrik Brink} and Dorthe Dahl-Jensen and Hubertus Fischer and Kumiko Goto-Azuma and Margareta Hansson and Johnsen, {Sigfus Johann} and Jean Jouzel and Val{\'e}rie Masson-Delmotte and Popp, {Trevor James} and Rasmussen, {Sune Olander} and Regine R{\"o}thlisberger and Urs Ruth and Bernhard Stauffer and Marie-Louise Siggaard-Andersen and Sveinbj{\"o}rnsd{\'o}ttir, {{\'A}rn{\'y} E.} and Anders Svensson and White, {James W.C.}",
note = "Paper id:: DOI: 10.1126/science.1157707",
year = "2008",
doi = "10.1126/science.1157707",
language = "English",
volume = "321",
pages = "680--684",
journal = "Science",
issn = "0036-8075",
publisher = "American Association for the Advancement of Science",

}

RIS

TY - JOUR

T1 - High-resolution Greenland Ice Core data show abrupt climate change happens in few years

AU - Steffensen, Jørgen Peder

AU - Andersen, Katrine Krogh

AU - Bigler, Matthias

AU - Clausen, Henrik Brink

AU - Dahl-Jensen, Dorthe

AU - Fischer, Hubertus

AU - Goto-Azuma, Kumiko

AU - Hansson, Margareta

AU - Johnsen, Sigfus Johann

AU - Jouzel, Jean

AU - Masson-Delmotte, Valérie

AU - Popp, Trevor James

AU - Rasmussen, Sune Olander

AU - Röthlisberger, Regine

AU - Ruth, Urs

AU - Stauffer, Bernhard

AU - Siggaard-Andersen, Marie-Louise

AU - Sveinbjörnsdóttir, Árný E.

AU - Svensson, Anders

AU - White, James W.C.

N1 - Paper id:: DOI: 10.1126/science.1157707

PY - 2008

Y1 - 2008

N2 - 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.

AB - 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.

U2 - 10.1126/science.1157707

DO - 10.1126/science.1157707

M3 - Journal article

C2 - 18566247

VL - 321

SP - 680

EP - 684

JO - Science

JF - Science

SN - 0036-8075

ER -

ID: 5347751