How warm was Greenland during the last interglacial period?

Landais, Amaelle; Masson-Delmotte, Valérie; Capron, Emilie ORCID: https://orcid.org/0000-0003-0784-1884; Langebroek, Petra M.; Bakker, Pepijn; Stone, Emma J.; Merz, Niklaus; Raible, Christoph C.; Fischer, Hubertus; Orsi, Anaïs; Prié, Frédéric; Vinther, Bo; Dahl-Jensen, Dorthe. 2016 How warm was Greenland during the last interglacial period? Climate of the Past, 12 (9). 1933-1948. https://doi.org/10.5194/cp-12-1933-2016

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Official URL: http://www.clim-past.net/12/1933/2016/

Abstract/Summary

The last interglacial period (LIG, ~ 129–116 thousand years ago) provides the most recent case study for multi-millennial polar warming above pre-industrial level and a respective response of the Greenland and Antarctic ice sheets to this warming, as well as a test bed for climate and ice sheet models. Past changes in Greenland ice sheet thickness and surface temperature during this period were recently derived from the NEEM ice core records, North-West Greenland. The NEEM paradox has emerged from an estimated large local warming above pre-industrial level (7.5 ± 1.8 °C at the deposition site 126 ka ago without correction for any overall ice sheet altitude changes between the LIG and pre-industrial) based on water isotopes, together with limited local ice thinning, suggesting more resilience of the real Greenland ice sheet than shown in some ice sheet models. Here, we provide an independent assessment of the average LIG Greenland surface warming using ice core air isotopic composition (δ15N) and relationships between accumulation rate and temperature. The LIG surface temperature at the upstream NEEM deposition site without ice sheet altitude correction is estimated to be warmer by +7 to +11 °C (+8 °C being the most likely estimate according to constraints on past accumulation rate) compared to the pre-industrial period. This temperature estimate is consistent with the 7.5 ± 1.8 °C warming initially determined from NEEM water isotopes. Moreover, we show that under such warm temperatures, melting of snow probably led to a significant firn shrinking by ~ 15 m. Climate simulations performed with present day ice sheet topography lead to much smaller warming but larger amplitudes (up to 5 °C) can be obtained from changes in sea ice extent and ice sheet topography. Still, ice sheet simulations forced by 5 °C surface warming lead to large ice sheet decay that are not compatible with existing data. Our new, independent temperature constrain therefore reinforces the NEEM paradox.

Item Type:	Publication - Article
Digital Object Identifier (DOI):	https://doi.org/10.5194/cp-12-1933-2016
Programmes:	BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate
ISSN:	1814-9359
Date made live:	12 Apr 2016 08:12 +0 (UTC)
URI:	https://nora.nerc.ac.uk/id/eprint/513415

Item Type:

Publication - Article

Digital Object Identifier (DOI):

https://doi.org/10.5194/cp-12-1933-2016

Programmes:

BAS Programmes > BAS Programmes 2015 > Ice Dynamics and Palaeoclimate

ISSN:

1814-9359

Date made live:

12 Apr 2016 08:12 +0 (UTC)

URI:

https://nora.nerc.ac.uk/id/eprint/513415