(Q55878591)

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Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes

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Influence of Bering Strait flow and North Atlantic circulation on glacial sea-level changes (English)

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Claire Waelbroeck

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Claire Waelbroeck

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Marie-France Loutre

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Marie-France Loutre

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Bette L. Otto‐Bliesner

3

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Bette L. Otto-Bliesner

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2

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Gerald A. Meehl

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Jerry X. Mitrovica

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Jerry X. Mitrovica

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7

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Kurt Lambeck

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Aixue Hu

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Weiqing Han

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Nan Rosenbloom

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publication date

10 January 2010

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Nature Geoscience

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3

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2

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118-121

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Late Quaternary ice sheet history of northern Eurasia

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Constraints on the Late Saalian to early Middle Weichselian ice sheet of Eurasia from field data and rebound modelling

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Quantifying ice-sheet feedbacks during the last glacial inception

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Sea level change through the last glacial cycle

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Climate change. North-south connections

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Investigating the Causes of the Response of the Thermohaline Circulation to Past and Future Climate Changes

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Evidence for general instability of past climate from a 250-kyr ice-core record

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Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years

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Heinrich events: Massive late Pleistocene detritus layers of the North Atlantic and their global climate imprint

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Meltwater pulse 1A from Antarctica as a trigger of the Bølling-Allerød warm interval

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Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming

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A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO2concentration

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Role of the Bering Strait in controlling North Atlantic ocean circulation and climate

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Response of Thermohaline Circulation to Freshwater Forcing under Present-Day and LGM Conditions

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The Community Climate System Model Version 3 (CCSM3)

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Does mean annual insolation have the potential to change the climate?

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Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

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Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years

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The Greenland ice sheet and greenhouse warming

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High-resolution record of Northern Hemisphere climate extending into the last interglacial period

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10.1038/NGEO729

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