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Younger Dryas ice-margin retreat in Greenland, new evidence from Southwest Green...
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Role of CO2 and Southern Ocean winds in glacial abrupt climate change
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Sea ice feedbacks influence the isotopic signature of Greenland ice sheet elevat...
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Significance of uncertain phasing between the onsets of stadial–interstadial tra...
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Decadal-scale progression of the onset of Dansgaard–Oeschger warming events
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Warm Greenland during the last interglacial: the role of regional changes in sea...
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Sea-ice feedbacks influence the isotopic signature of Greenland Ice Sheet elevat...
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Effects of LGM sea surface temperature and sea ice extent on the isotope-tempera...
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Methanesulfonic acid (MSA) migration in polar ice: data synthesis and theory
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Water isotopes – climate relationships for the mid-Holocene and preindustrial pe...
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High-frequency climate variability in the Holocene from a coastal-dome ice core...
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Sea ice as a source of sea salt aerosol to Greenland ice cores: a model-based st...
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Climate information preserved in seasonal water isotope at NEEM: relationships w...
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Geochronological reconsideration of the eastern European key loess section at St...
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Greenland during the last interglacial: the relative importance of insolation an...
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Laminated sediments in the Bering Sea reveal atmospheric teleconnections to Gree...
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Sea ice and pollution-modulated changes in Greenland ice core methanesulfonate a...
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High-frequency climate oscillations in the Holocene from a coastal-dome ice core...
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Effects of Last Glacial Maximum (LGM) sea surface temperature and sea ice extent...
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A statistical approach to the phasing of atmospheric reorganization and sea ice...
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