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Antarctic ice: going, going, gone?
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Sea-ice proxies in Antarctic ice cores
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Tropical Pacific variability and anthropogenic forcing are the key drivers of th...
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Century-scale perspectives on observed and simulated Southern Ocean sea ice tren...
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The preservation of methanesulphonic acid in frozen ice-core samples
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A review of sea ice proxy information from polar ice cores
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Variability of sea-ice in the northern Weddell Sea during the 20th century
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NOAA/WDS Paleoclimatology - Colle Gnifetti 275 Year Ice Core Black Carbon and Ch...
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Evolution of the Southern Annular Mode during the past millennium
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Automated ice-core layer-counting with strong univariate signals
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Automated ice-core layer-counting with strong univariate signals
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Automated ice-core layer-counting with strong univariate signals
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Automated ice-core layer-counting with strong univariate signals
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Automated ice-core layer-counting with strong univariate signals
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Acceleration of snow melt in an Antarctic Peninsula ice core during the twentiet...
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NOAA/WDS Paleoclimatology - James Ross Island, Antarctica Ice Core 2000 Year Ann...
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Solve Antarctica's sea-ice puzzle
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Antarctic climate variability on regional and continental scales over the last 2...
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El Niño–Southern Oscillation signal in a new East Antarctic ice core, Mount Brow...
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NOAA/WDS Paleoclimatology - PAGES Antarctica2k Temperature Reconstructions
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