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1-D-ice flow modelling at EPICA Dome C and Dome Fuji, East Antarctica

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TLDR
One-dimensional (1-D) ice flow models are used to construct the age scales at the Dome C and Dome Fuji drilling sites (East Antarctica) as discussed by the authors, where poorly constrained glaciological parameters at each site are recovered by fitting independent age markers identified within each core.
Abstract
One-dimensional (1-D) ice flow models are used to construct the age scales at the Dome C and Dome Fuji drilling sites (East Antarctica) The poorly constrained glaciological parameters at each site are recovered by fitting independent age markers identified within each core We reconstruct past accumulation rates, that are larger than those modelled using the classical vapour saturation pressure relationship during glacial periods by up to a factor 15 During the Early Holocene, changes in reconstructed accumulation are not linearly related to changes in ice isotopic composition A simple model of past elevation changes is developed and shows an amplitude variation of 110–120 m at both sites We suggest that there is basal melting at Dome C (056±019 mm/yr) The reconstructed velocity profile is highly non-linear at both sites, which suggests complex ice flow effects This induces a non-linear thinning function in both drilling sites, which is also characterized by bumps corresponding to variations in ice thickness with time

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Orbital and millenial antarctic climate variability over the last 800 000 years

TL;DR: A high-resolution deuterium profile is available along the entire European Project for Ice Coring in Antarctica Dome C ice core, extending this climate record back to marine isotope stage 20.2, ∼800,000 years ago.
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A reconciled estimate of ice-sheet mass balance

TL;DR: There is good agreement between different satellite methods—especially in Greenland and West Antarctica—and that combining satellite data sets leads to greater certainty, and the mass balance of Earth’s polar ice sheets is estimated by combining the results of existing independent techniques.
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Target atmospheric CO2: Where should humanity aim?

TL;DR: In this paper, the authors show that the current CO2 level can be reduced to at most 350 ppm by phasing out coal use except where CO2 is captured and adopting agricultural and forestry practices that sequester carbon.
References
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Journal ArticleDOI

A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

TL;DR: In this paper, a 53-Myr stack (LR04) of benthic δ18O records from 57 globally distributed sites aligned by an automated graphic correlation algorithm is presented.
Journal ArticleDOI

Timing of Millennial-Scale Climate Change in Antarctica and Greenland During the Last Glacial Period

TL;DR: A precise relative chronology for Greenland and West Antarctic paleotemperature is extended to 90,000 years ago, based on correlation of atmospheric methane records from the Greenland Ice Sheet Project 2 and Byrd ice cores, to provide further evidence for the operation of a "bipolar see-saw" in air temperatures and an oceanic teleconnection between the hemispheres on millennial time scales.
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