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A. Landais
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Temperature reconstruction from 10 to 120 kyr b2k from the NGRIP ice core
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Recent changes in north-west Greenland climate documented by NEEM shallow ice co...
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What controls the isotopic composition of Greenland surface snow?
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A comparison of the present and last interglacial periods in six Antarctic ice c...
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Persistent influence of ice sheet melting on high northern latitude climate duri...
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Bipolar volcanic synchronization of abrupt climate change in Greenland and Antar...
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An optimized multi-proxy, multi-site Antarctic ice and gas orbital chronology (A...
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On the gas-ice depth difference (Δdepth) along the EPICA Dome C ice core
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How warm was Greenland during the last interglacial period?
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On the similarity and apparent cycles of isotopic variations in East Antarctic s...
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The Antarctic ice core chronology (AICC2012): an optimized multi-parameter and m...
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Ranges of moisture-source temperature estimated from Antarctic ice cores stable...
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Analytical constraints on layered gas trapping and smoothing of atmospheric vari...
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Acquisition of isotopic composition for surface snow in East Antarctica and the...
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Retrieving the paleoclimatic signal from the deeper part of the EPICA Dome C ice...
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Phase relationships between orbital forcing and the composition of air trapped i...
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Past temperature reconstructions from deep ice cores: relevance for future clima...
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Deglaciation records of 17O-excess in East Antarctica: reliable reconstruction o...
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Comparing past accumulation rate reconstructions in East Antarctic ice cores usi...
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Millennial-scale atmospheric CO2 variations during the Marine Isotope Stage 6 pe...
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A. Landais
V. Masson-Delmotte
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geo
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