The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr

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Standard

The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr. / Nielsen, Lisbeth Tangaa; Adalgeirsdottir, Gudfinna; Gkinis, Vasileios; Nuterman, Roman; Hvidberg, Christine Schøtt.

I: Journal of Glaciology, Bind 64, Nr. 245, 22.05.2018, s. 477-488.

Publikation: Bidrag til tidsskrift › Tidsskriftartikel › Forskning › fagfællebedømt

Harvard

Nielsen, LT, Adalgeirsdottir, G, Gkinis, V, Nuterman, R & Hvidberg, CS 2018, 'The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr', Journal of Glaciology, bind 64, nr. 245, s. 477-488. https://doi.org/10.1017/jog.2018.40

APA

Nielsen, L. T., Adalgeirsdottir, G., Gkinis, V., Nuterman, R., & Hvidberg, C. S. (2018). The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr. Journal of Glaciology, 64(245), 477-488. https://doi.org/10.1017/jog.2018.40

Vancouver

Nielsen LT, Adalgeirsdottir G, Gkinis V, Nuterman R, Hvidberg CS. The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr. Journal of Glaciology. 2018 maj 22;64(245):477-488. https://doi.org/10.1017/jog.2018.40

Author

Nielsen, Lisbeth Tangaa ; Adalgeirsdottir, Gudfinna ; Gkinis, Vasileios ; Nuterman, Roman ; Hvidberg, Christine Schøtt. / The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr. I: Journal of Glaciology. 2018 ; Bind 64, Nr. 245. s. 477-488.

Bibtex

@article{ad6c4a0cd6104cfdaa119b95ef5d5c1a,
title = "The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr",
abstract = "The Holocene climatic optimum was a period 8–5 kyr ago when annual mean surface temperatures in Greenland were 2–3°C warmer than present-day values. However, this warming left little imprint on commonly used temperature proxies often used to derive the climate forcing for simulations of the past evolution of the Greenland ice sheet. In this study, we investigate the evolution of the Greenland ice sheet through the Holocene when forced by different proxy-derived temperature histories from ice core records, focusing on the effect of sustained higher surface temperatures during the early Holocene. We find that the ice sheet retreats to a minimum volume of ~0.15–1.2 m sea-level equivalent smaller than present in the early or mid-Holocene when forcing an ice-sheet model with temperature reconstructions that contain a climatic optimum, and that the ice sheet has continued to recover from this minimum up to present day. Reconstructions without a warm climatic optimum in the early Holocene result in smaller ice losses continuing throughout the last 10 kyr. For all the simulated ice-sheet histories, the ice sheet is approaching a steady state at the end of the 20th century.",
author = "Nielsen, {Lisbeth Tangaa} and Gudfinna Adalgeirsdottir and Vasileios Gkinis and Roman Nuterman and Hvidberg, {Christine Sch{\o}tt}",
year = "2018",
month = may,
day = "22",
doi = "10.1017/jog.2018.40",
language = "English",
volume = "64",
pages = "477--488",
journal = "Journal of Glaciology",
issn = "0022-1430",
publisher = "International Glaciological Society",
number = "245",

}

RIS

TY - JOUR

T1 - The effect of a Holocene climatic optimum on the evolution of the Greenland ice sheet during the last 10 kyr

AU - Nielsen, Lisbeth Tangaa

AU - Adalgeirsdottir, Gudfinna

AU - Gkinis, Vasileios

AU - Nuterman, Roman

AU - Hvidberg, Christine Schøtt

PY - 2018/5/22

Y1 - 2018/5/22

N2 - The Holocene climatic optimum was a period 8–5 kyr ago when annual mean surface temperatures in Greenland were 2–3°C warmer than present-day values. However, this warming left little imprint on commonly used temperature proxies often used to derive the climate forcing for simulations of the past evolution of the Greenland ice sheet. In this study, we investigate the evolution of the Greenland ice sheet through the Holocene when forced by different proxy-derived temperature histories from ice core records, focusing on the effect of sustained higher surface temperatures during the early Holocene. We find that the ice sheet retreats to a minimum volume of ~0.15–1.2 m sea-level equivalent smaller than present in the early or mid-Holocene when forcing an ice-sheet model with temperature reconstructions that contain a climatic optimum, and that the ice sheet has continued to recover from this minimum up to present day. Reconstructions without a warm climatic optimum in the early Holocene result in smaller ice losses continuing throughout the last 10 kyr. For all the simulated ice-sheet histories, the ice sheet is approaching a steady state at the end of the 20th century.

AB - The Holocene climatic optimum was a period 8–5 kyr ago when annual mean surface temperatures in Greenland were 2–3°C warmer than present-day values. However, this warming left little imprint on commonly used temperature proxies often used to derive the climate forcing for simulations of the past evolution of the Greenland ice sheet. In this study, we investigate the evolution of the Greenland ice sheet through the Holocene when forced by different proxy-derived temperature histories from ice core records, focusing on the effect of sustained higher surface temperatures during the early Holocene. We find that the ice sheet retreats to a minimum volume of ~0.15–1.2 m sea-level equivalent smaller than present in the early or mid-Holocene when forcing an ice-sheet model with temperature reconstructions that contain a climatic optimum, and that the ice sheet has continued to recover from this minimum up to present day. Reconstructions without a warm climatic optimum in the early Holocene result in smaller ice losses continuing throughout the last 10 kyr. For all the simulated ice-sheet histories, the ice sheet is approaching a steady state at the end of the 20th century.

U2 - 10.1017/jog.2018.40

DO - 10.1017/jog.2018.40

M3 - Journal article

VL - 64

SP - 477

EP - 488

JO - Journal of Glaciology

JF - Journal of Glaciology

SN - 0022-1430

IS - 245

ER -

ID: 197000892