East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat.

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

Standard

East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat. / Simonsen, Marius Folden; Baccolo, Giovanni; Blunier, Thomas; Borunda, Alejandra; Delmonte, Barbara; Frei, Robert; Goldstein, Steven; Grinsted, Aslak; Kjær, Helle Astrid; Sowers, Todd; Svensson, Anders; Vinther, Bo; Vladimirova, Diana; Winckler, Gisela; Winstrup, Mai; Vallelonga, Paul.

In: Nature Communications, Vol. 10, 4494, 03.10.2019.

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

Harvard

Simonsen, MF, Baccolo, G, Blunier, T, Borunda, A, Delmonte, B, Frei, R, Goldstein, S, Grinsted, A, Kjær, HA, Sowers, T, Svensson, A, Vinther, B, Vladimirova, D, Winckler, G, Winstrup, M & Vallelonga, P 2019, 'East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat.', Nature Communications, vol. 10, 4494. https://doi.org/10.1038/s41467-019-12546-2

APA

Simonsen, M. F., Baccolo, G., Blunier, T., Borunda, A., Delmonte, B., Frei, R., Goldstein, S., Grinsted, A., Kjær, H. A., Sowers, T., Svensson, A., Vinther, B., Vladimirova, D., Winckler, G., Winstrup, M., & Vallelonga, P. (2019). East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat. Nature Communications, 10, [4494]. https://doi.org/10.1038/s41467-019-12546-2

Vancouver

Simonsen MF, Baccolo G, Blunier T, Borunda A, Delmonte B, Frei R et al. East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat. Nature Communications. 2019 Oct 3;10. 4494. https://doi.org/10.1038/s41467-019-12546-2

Author

Simonsen, Marius Folden ; Baccolo, Giovanni ; Blunier, Thomas ; Borunda, Alejandra ; Delmonte, Barbara ; Frei, Robert ; Goldstein, Steven ; Grinsted, Aslak ; Kjær, Helle Astrid ; Sowers, Todd ; Svensson, Anders ; Vinther, Bo ; Vladimirova, Diana ; Winckler, Gisela ; Winstrup, Mai ; Vallelonga, Paul. / East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat. In: Nature Communications. 2019 ; Vol. 10.

Bibtex

@article{9fff5f6fce9245c6950b77af65a10b20,
title = "East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat.",
abstract = "Accurate estimates of the past extent of the Greenland ice sheet provide critical constraints for ice sheet models used to determine Greenland{\textquoteright}s response to climate forcing and contribution to global sea level. Here we use a continuous ice core dust record from the Renland ice cap on the east coast of Greenland to constrain the timing of changes to the ice sheet margin and relative sea level over the last glacial cycle. During the Holocene and the previous interglacial period (Eemian) the dust record was dominated by coarse particles consistent with rock samples from central East Greenland. From the coarse particle concentration record we infer the East Greenland ice sheet margin advanced from 113.4 ± 0.4 to 111.0 ± 0.4 ka BP during the glacial onset and retreated from 12.1 ± 0.1 to 9.0 ± 0.1 ka BP during the last deglaciation. These findings constrain the possible response of the Greenland ice sheet to climate forcings.",
author = "Simonsen, {Marius Folden} and Giovanni Baccolo and Thomas Blunier and Alejandra Borunda and Barbara Delmonte and Robert Frei and Steven Goldstein and Aslak Grinsted and Kj{\ae}r, {Helle Astrid} and Todd Sowers and Anders Svensson and Bo Vinther and Diana Vladimirova and Gisela Winckler and Mai Winstrup and Paul Vallelonga",
year = "2019",
month = oct,
day = "3",
doi = "10.1038/s41467-019-12546-2",
language = "English",
volume = "10",
journal = "Nature Communications",
issn = "2041-1723",
publisher = "nature publishing group",

}

RIS

TY - JOUR

T1 - East Greenland ice core dust record reveals timing of Greenland ice sheet advance and retreat.

AU - Simonsen, Marius Folden

AU - Baccolo, Giovanni

AU - Blunier, Thomas

AU - Borunda, Alejandra

AU - Delmonte, Barbara

AU - Frei, Robert

AU - Goldstein, Steven

AU - Grinsted, Aslak

AU - Kjær, Helle Astrid

AU - Sowers, Todd

AU - Svensson, Anders

AU - Vinther, Bo

AU - Vladimirova, Diana

AU - Winckler, Gisela

AU - Winstrup, Mai

AU - Vallelonga, Paul

PY - 2019/10/3

Y1 - 2019/10/3

N2 - Accurate estimates of the past extent of the Greenland ice sheet provide critical constraints for ice sheet models used to determine Greenland’s response to climate forcing and contribution to global sea level. Here we use a continuous ice core dust record from the Renland ice cap on the east coast of Greenland to constrain the timing of changes to the ice sheet margin and relative sea level over the last glacial cycle. During the Holocene and the previous interglacial period (Eemian) the dust record was dominated by coarse particles consistent with rock samples from central East Greenland. From the coarse particle concentration record we infer the East Greenland ice sheet margin advanced from 113.4 ± 0.4 to 111.0 ± 0.4 ka BP during the glacial onset and retreated from 12.1 ± 0.1 to 9.0 ± 0.1 ka BP during the last deglaciation. These findings constrain the possible response of the Greenland ice sheet to climate forcings.

AB - Accurate estimates of the past extent of the Greenland ice sheet provide critical constraints for ice sheet models used to determine Greenland’s response to climate forcing and contribution to global sea level. Here we use a continuous ice core dust record from the Renland ice cap on the east coast of Greenland to constrain the timing of changes to the ice sheet margin and relative sea level over the last glacial cycle. During the Holocene and the previous interglacial period (Eemian) the dust record was dominated by coarse particles consistent with rock samples from central East Greenland. From the coarse particle concentration record we infer the East Greenland ice sheet margin advanced from 113.4 ± 0.4 to 111.0 ± 0.4 ka BP during the glacial onset and retreated from 12.1 ± 0.1 to 9.0 ± 0.1 ka BP during the last deglaciation. These findings constrain the possible response of the Greenland ice sheet to climate forcings.

U2 - 10.1038/s41467-019-12546-2

DO - 10.1038/s41467-019-12546-2

M3 - Journal article

C2 - 31582753

VL - 10

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

M1 - 4494

ER -

ID: 228534480