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Where to Find 1.5 Million Yr Old Ice for the Ipics Oldest Ice Ice Core : Volume 9, Issue 3 (27/05/2013)

By Fischer, H.

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Book Id: WPLBN0003982332
Format Type: PDF Article :
File Size: Pages 45
Reproduction Date: 2015

Title: Where to Find 1.5 Million Yr Old Ice for the Ipics Oldest Ice Ice Core : Volume 9, Issue 3 (27/05/2013)  
Author: Fischer, H.
Volume: Vol. 9, Issue 3
Language: English
Subject: Science, Climate, Past
Collections: Periodicals: Journal and Magazine Collection (Contemporary), Copernicus GmbH
Publication Date:
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications


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Severinghaus, J., Brook, E., Frezzotti, M., Dahl-Jensen, D., Steinhage, D., Gallee, H.,...Hudspeth, D. (2013). Where to Find 1.5 Million Yr Old Ice for the Ipics Oldest Ice Ice Core : Volume 9, Issue 3 (27/05/2013). Retrieved from

Description: Climate and Environmental Physics, Physics Institute, University of Bern, Sidlerstrasse 5, 3012 Bern and Oeschger Centre for Climate Change Research, University of Bern, Bern, Switzerland. The recovery of a 1.5 Myr long ice core from Antarctica represents a keystone to our understanding of Quaternary climate, the progression of glaciation over this time period and the role of greenhouse gas cycles in this progression. Here we show that such old ice is most likely to exist in the plateau area of the East Antarctic Ice Sheet (EAIS) without stratigraphic disturbance and should be able to be recovered after careful pre-site selection studies. Based on a simple ice and heat flow model and glaciological observations, we conclude that positions in the vicinity of major domes and saddle positions on the East Antarctic Plateau will most likely have such old ice in store and represent the best study areas for dedicated reconnaissance studies in the near future. In contrast to previous ice core drill site selections, we strongly argue for significantly reduced ice thickness to avoid bottom melting, while at the same time maximizing the resolution and the distance of such old ice to the bedrock. For example for the geothermal heat flux and accumulation conditions at Dome C, an ice thickness lower than 2500 m would be required to find 1.5 Myr old ice. However, the final choice is strongly dependent on the local geothermal heat flux, which is largely unknown for the EAIS and has to be determined beforehand. In addition, the detailed bedrock topography and ice flow history for candidates of an Oldest Ice ice coring site has to be reconstructed. Finally, we argue strongly for rapid access drilling before any full deep ice coring activity commences to bring datable samples to the surface and to allow an age check of the oldest ice.

Where to find 1.5 million yr old ice for the IPICS Oldest Ice ice core

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