(Q56804403)

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Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas Event

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scholarly article

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Coupled ocean-atmosphere model response to freshwater input: Comparison to Younger Dryas Event (English)

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1 reference

based on heuristic

inferred from title

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1

object named as

Syukuro Manabe

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Ronald J. Stouffer

2

object named as

Ronald J. Stouffer

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publication date

April 1997

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Paleoceanography

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12

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2

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321-336

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Evidence for massive discharges of icebergs into the North Atlantic ocean during the last glacial period

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North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature

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A numerical investigation of the oceanic general circulation

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A possible younger dryas record in southeastern alaska

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Climate instability during the last interglacial period recorded in the GRIP ice core

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Tropical temperature variations since 20,000 years ago: modulating interhemispheric climate change

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Simulation of abrupt climate change induced by freshwater input to the North Atlantic Ocean

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Climate Change During the Last Deglaciation in Antarctica

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Global Younger Dryas?

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Rapid climate transitions in a coupled ocean–atmosphere model

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Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle

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Late glacial stage and holocene tropical ice core records from huascaran, peru

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Climate records covering the last deglaciation

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Synchronous changes in atmospheric CH4 and Greenland climate between 40 and 8 kyr BP

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Deglacial sea-level record from Tahiti corals and the timing of global meltwater discharge

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Does the ocean–atmosphere system have more than one stable mode of operation?

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A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation

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Century-scale effects of increased atmospheric C02 on the ocean–atmosphere system

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Interhemispheric asymmetry in climate response to a gradual increase of atmospheric CO2

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The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas Event

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Origin of the first global meltwater pulse following the Last Glacial Maximum

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Interdecadal Variations of the Thermohaline Circulation in a Coupled Ocean-Atmosphere Model

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Multidecadal climate variability in the Greenland Sea and surrounding regions: A coupled model simulation

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Younger dryas age advance of franz josef glacier in the southern alps of new zealand

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A Reevaluation of the Timing and Causes of High Lake Phases in the Lake Michigan Basin

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Glacial-Holocene stratigraphy, chronology, and paleoceanographic observations on some North Atlantic sediment drifts

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Deglacial meltwater discharge, North Atlantic Deep Circulation, and abrupt climate change

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Evidence for a Younger Dryas-like cooling event on the British Columbia coast

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Multiple-Century Response of a Coupled Ocean-Atmosphere Model to an Increase of Atmospheric Carbon Dioxide

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Two Stable Equilibria of a Coupled Ocean-Atmosphere Model

1 reference

11 October 2022

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Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation

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Stability and Variability of the Thermohaline Circulation

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Identifiers

10.1029/96PA03932

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1997PalOc..12..321M

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