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Antarctic and global climate history viewed from ice cores

Nature (London), 2018-06, Vol.558 (7709), p.200-208

2018

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Siple Dome ice reveals two modes of millennial CO2 change during the last ice age

Nature communications, 2014-04, Vol.5 (1), p.3723, Article 3723

2014

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Abrupt changes in the global carbon cycle during the last glacial period

Nature geoscience, 2021-02, Vol.14 (2), p.91-96

2021

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Reconciling ice core CO2 and land-use change following New World-Old World contact

Nature communications, 2024-03, Vol.15 (1), p.1735-1735, Article 1735

2024

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Centennial-scale changes in the global carbon cycle during the last deglaciation

Nature (London), 2014-10, Vol.514 (7524), p.616-619

2014

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Greenland temperature response to climate forcing during the last deglaciation

Science (American Association for the Advancement of Science), 2014-09, Vol.345 (6201), p.1177-1180

2014

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Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation

Proceedings of the National Academy of Sciences - PNAS, 2016-03, Vol.113 (13), p.3465-3470

2016

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Enhanced tropical methane production in response to iceberg discharge in the North Atlantic

Science (American Association for the Advancement of Science), 2015-05, Vol.348 (6238), p.1016-1019

2015

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Reconstructing the last interglacial at Summit, Greenland: Insights from GISP2

Proceedings of the National Academy of Sciences - PNAS, 2016-08, Vol.113 (35), p.9710-9715

2016

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

Science (American Association for the Advancement of Science), 2001-01, Vol.291 (5501), p.109-112

2001

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The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP)

Climate of the past, 2016-03, Vol.12 (3), p.769-786

2016

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Precise timing and characterization of abrupt climate change 8200 years ago from air trapped in polar ice

Quaternary science reviews, 2007-05, Vol.26 (9), p.1212-1222

2007

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Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

Proceedings of the National Academy of Sciences - PNAS, 2017-09, Vol.114 (38), p.10035-10040

2017

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Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4

Nature communications, 2022-09, Vol.13 (1), p.5443-5443, Article 5443

2022

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Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent

Geophysical research letters, 2014-08, Vol.41 (15), p.5514-5521

2014

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Antarctic evidence for an abrupt northward shift of the Southern Hemisphere westerlies at 32 ka BP

Nature communications, 2023-09, Vol.14 (1), p.5432-5432, Article 5432

2023

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Radiometric ⁸¹Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica

Proceedings of the National Academy of Sciences - PNAS, 2014-05, Vol.111 (19), p.6876-6881

2014

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Observing and modeling the influence of layering on bubble trapping in polar firn

Journal of geophysical research. Atmospheres, 2015-03, Vol.120 (6), p.2558-2574

2015

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Continuous methane measurements from a late Holocene Greenland ice core: Atmospheric and in-situ signals

Earth and planetary science letters, 2013-04, Vol.368, p.9-19

2013

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Atmospheric CO2 over the last 1000 years: A high-resolution record from the West Antarctic Ice Sheet (WAIS) Divide ice core

Global biogeochemical cycles, 2012-06, Vol.26 (2), p.n/a

2012

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Atmospheric methane control mechanisms during the early Holocene

Climate of the past, 2017-09, Vol.13 (9), p.1227-1242

2017

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Abrupt Climate Change at the End of the Last Glacial Period Inferred from Trapped Air in Polar Ice

Science (American Association for the Advancement of Science), 1999-10, Vol.286 (5441), p.930-934

1999

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Geochemical Proxies of North American Freshwater Routing during the Younger Dryas Cold Event

Proceedings of the National Academy of Sciences - PNAS, 2007-04, Vol.104 (16), p.6556-6561

2007

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Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation

Nature (London), 2014-12, Vol.516 (7530), p.234-237

2014

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Antarctic and global climate history viewed from ice cores

Siple Dome ice reveals two modes of millennial CO2 change during the last ice age

Abrupt changes in the global carbon cycle during the last glacial period

Reconciling ice core CO2 and land-use change following New World-Old World contact

Centennial-scale changes in the global carbon cycle during the last deglaciation

Greenland temperature response to climate forcing during the last deglaciation

Carbon isotopes characterize rapid changes in atmospheric carbon dioxide during the last deglaciation

Enhanced tropical methane production in response to iceberg discharge in the North Atlantic

Reconstructing the last interglacial at Summit, Greenland: Insights from GISP2

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

The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP)

Precise timing and characterization of abrupt climate change 8200 years ago from air trapped in polar ice

Synchronous volcanic eruptions and abrupt climate change ∼17.7 ka plausibly linked by stratospheric ozone depletion

Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4

Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent

Antarctic evidence for an abrupt northward shift of the Southern Hemisphere westerlies at 32 ka BP

Radiometric ⁸¹Kr dating identifies 120,000-year-old ice at Taylor Glacier, Antarctica

Observing and modeling the influence of layering on bubble trapping in polar firn

Continuous methane measurements from a late Holocene Greenland ice core: Atmospheric and in-situ signals

Atmospheric CO2 over the last 1000 years: A high-resolution record from the West Antarctic Ice Sheet (WAIS) Divide ice core

Atmospheric methane control mechanisms during the early Holocene

Abrupt Climate Change at the End of the Last Glacial Period Inferred from Trapped Air in Polar Ice

Geochemical Proxies of North American Freshwater Routing during the Younger Dryas Cold Event

Isotopic constraints on marine and terrestrial N2O emissions during the last deglaciation

The new Kr-86 excess ice core proxy for synoptic activity: West Antarctic storminess possibly linked to Intertropical Convergence Zone (ITCZ) movement through the last deglaciation

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