Mechanisms for climate variability during glacial and interglacial periods

No abstract is available for this paper.

• Publication year

  2005

• Venue

  Paleoceanography

• Publication date

  2005-12-01

• Fields of study

  Geology, Physics, Environmental Science

• Identifiers
  DOI 10.1029/2004PA001113
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

• A “Triple Sea-Ice State” Mechanism for the Abrupt Warming and Synchronous Ice Sheet Collapses During Heinrich Events

  2004influential reference
• Thermohaline circulation: The current climate

  2003influential reference
• Glacial North Atlantic: Sea-surface conditions reconstructed by GLAMAP 2000

  2003cited by this paper
• Sea-ice switches and abrupt climate change

  2003influential reference
• Ocean circulation and climate during the past 120,000 years

  2002influential reference
• The role of the thermohaline circulation in abrupt climate change

  2002influential reference
• Global distribution of centennial-scale records for Marine Isotope Stage (MIS) 3: a database

  2001cited by this paper
• Stochastic resonance in the North Atlantic

  2001influential reference
• Climate Swings Come into Focus

  2001influential reference
• Rapid changes of glacial climate simulated in a coupled climate model

  2001influential reference
• Improved estimates of global ocean circulation, heat transport and mixing from hydrographic data

  2000cited by this paper
• Sea-ice cover, sea-surface salinity and halo-/thermocline structure of the northwest North Atlantic: modern versus full glacial conditions

  2000cited by this paper
• Glacial thermohaline circulation states of the northern Atlantic: the compatibility of modelling and observations

  2000cited by this paper
• Reduced North Atlantic Deep Water flux to the glacial Southern Ocean inferred from neodymium isotope ratios

  2000cited by this paper
• Sea ice as the glacial cycles' climate switch: Role of seasonal and orbital forcing

  2000cited by this paper
• Large-Scale Circulation and Production of Stratification: Effects of Wind, Geometry, and Diffusion

  2000cited by this paper
• Reconstruction of sea-surface temperature, salinity, and sea-ice cover in the northern North Atlantic during the last glacial maximum based on dinocyst assemblages

  2000cited by this paper
• Warming of the tropical Atlantic Ocean and slowdown of thermohaline circulation during the last deglaciation

  1999cited by this paper
• Holocene periodicity in North Atlantic climate and deep-ocean flow south of Iceland

  1999cited by this paper
• A Dynamical Systems Model of the Dansgaard–Oeschger Oscillation and the Origin of the Bond Cycle

  1999influential reference
• Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice

  1998cited by this paper
• Sea ice effects on the sensitivity of the thermohaline circulation in simplified atmosphere-ocean-sea ice models

  1998cited by this paper
• On the Ocean’s Large-Scale Circulation near the Limit of No Vertical Mixing

  1998cited by this paper
• Coupled ocean‐atmosphere model response to freshwater input: Comparison to Younger Dryas Event

  1997influential reference
• Inherently unstable climate behaviour due to weak thermohaline ocean circulation

  1997cited by this paper
• Large-scale circulation with small diapycnal diffusion: The two-thermocline limit

  1997influential reference
• The effect of cold climate upon North Atlantic Deep Water formation in a simple ocean-atmosphere model

  1997cited by this paper
• A Pervasive Millennial-Scale Cycle in North Atlantic Holocene and Glacial Climates

  1997cited by this paper
• Dansgaard–Oeschger Oscillations in a Coupled Atmosphere–Ocean Climate Model

  1997influential reference
• A simple friction and diffusion scheme for planetary geostrophic basin models

  1997cited by this paper
• Glacial Climate in the Tropics

  1996cited by this paper
• An atmospheric energy-moisture balance model: Climatology, interpentadal climate change, and coupling to an ocean general circulation model

  1996cited by this paper
• Simulation of abrupt climate change induced by freshwater input to the North Atlantic Ocean

  1995influential reference
• Suborbital timescale variability of North Atlantic Deep Water during the past 200

  1995influential reference
• Deep circulation change linked to HEINRICH Event 1 and Younger Dryas in a middepth North Atlantic Core

  1994influential reference
• The role of the deep ocean in North Atlantic climate change between 70 and 130 kyr ago

  1994influential reference
• Rapid climate transitions in a coupled ocean–atmosphere model

  1994cited by this paper
• Western North Atlantic evidence for millennial-scale changes in ocean circulation and climate

  1994cited by this paper
• Climate correlations between Greenland and Antarctica during the past 100,000 years

  1994influential reference
• The ‘flickering switch’ of late Pleistocene climate change

  1993influential reference
• Evidence for general instability of past climate from a 250-kyr ice-core record

  1993influential reference
• Extending the Vostok ice-core record of palaeoclimate to the penultimate glacial period

  1993cited by this paper
• Correlations between climate records from North Atlantic sediments and Greenland ice

  1993cited by this paper
• Mid-Depth Circulation of the Subpolar North Atlantic During the Last Glacial Maximum

  1993influential reference
• Deep Decoupling Oscillations of the Oceanic Thermohaline Circulation

  1993cited by this paper
• Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich events

  1993influential reference
• Irregular glacial interstadials recorded in a new Greenland ice core

  1992influential reference
• Freshwater flux forcing of decadal and interdecadal oceanic variability

  1991influential reference
• Rapid transitions of the ocean's deep circulation induced by changes in surface water fluxes

  1991influential reference
• Surface salinity reconstruction of the north-atlantic ocean during the last glacial maximum

  1991cited by this paper
• A salt oscillator in the glacial Atlantic? 1. The concept

  1990influential reference
• Deepwater source variations during the last climatic cycle and their impact on the global deepwater circulation

  1988cited by this paper
• Origin and Consequences of Cyclic Ice Rafting in the Northeast Atlantic Ocean During the Past 130,000 Years

  1988influential reference
• Two Stable Equilibria of a Coupled Ocean-Atmosphere Model

  1988influential reference
• North Atlantic thermohaline circulation during the past 20,000 years linked to high-latitude surface temperature

  1987cited by this paper
• How many nuclear reactor accidents?

  1987cited by this paper
• High-latitude salinity effects and interhemispheric thermohaline circulations

  1986cited by this paper
• Comparison of Atlantic and Pacific paleochemical records for the last 215,000 years : changes in deep ocean circulation and chemical inventories

  1985cited by this paper
• A large-scale numerical model of sea ice

  1979cited by this paper
• The surface of the ice-age Earth.

  1976cited by this paper
• A MODEL FOR THE THERMODYNAMIC GROWTH OF SEA ICE IN NUMERICAL INVESTIGATIONS OF CLIMATE

  1975cited by this paper
• Late Cenozoic Evolution of the Cape Coast Between Knysna and Cape St. Francis, South Africa

  1972cited by this paper
• Thermohaline Convection with Two Stable Regimes of Flow

  1961cited by this paper
• Variations in Atlantic surface ocean paleoceanography , 50 ø-80 øN : A time-slice record of the last 30 , 000 years

  year unknowncited by this paper

• Summer amplification of interannual variability changes in surface air temperature during the last interglacial period

  2025cites this paper
• Surface buoyancy control of millennial-scale variations in the Atlantic meridional ocean circulation

  2024cites this paper
• Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials? Implications from hosing experiments

  2021cites this paper
• Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials?

  2021cites this paper
• Feedbacks Driving Interdecadal Variability in Southern Ocean Convection in Climate Models: A Coupled Oscillator Mechanism

  2020cites this paper
• Roles of Sea Ice–Surface Wind Feedback in Maintaining the Glacial Atlantic Meridional Overturning Circulation and Climate

  2020cites this paper
• Roles of Sea Ice–Surface Wind Feedback in Maintaining the Glacial Atlantic Meridional Overturning Circulation and Climate

  2020cites this paper
• Impact of mid-glacial ice sheets on deep ocean circulation and global climate

  2020cites this paper
• Transitions and oscillations in a thermohaline deep ocean circulation model

  2018cites this paper
• Ocean circulation, ice shelf, and sea ice interactions explain Dansgaard–Oeschger cycles

  2018cites this paper
• Basin‐Width Dependence of Northern Deep Convection

  2017cites this paper
• Unhosed : interruptions of the Atlantic Meridional Overturning in a global coupled model , with and without freshwater forcing

  2016cites this paper
• Hosed vs. unhosed: interruptions of the Atlantic Meridional Overturning Circulation in a global coupled model, with and without freshwater forcing

  2016cites this paper
• Low-frequency climate variability of an aquaplanet

  2015cites this paper
• Hosed vs. unhosed: global response to interruptions of the Atlantic Meridional Overturning, with and without freshwater forcing

  2015cites this paper
• Instability of the Atlantic overturning circulation during Marine Isotope Stage 3

  2014cites this paper
• A Heuristic Model of Dansgaard–Oeschger Cycles. Part I: Description, Results, and Sensitivity Studies

  2014cites this paper
• Multiple sea-ice states and abrupt MOC transitions in a general circulation ocean model

  2013cites this paper
• The Role of Oceans and Sea Ice in Abrupt Transitions between Multiple Climate States

  2013influential citation
• Wind-stress feedback amplification of abrupt millennial-scale climate changes

  2013cites this paper
• Modeling Abrupt Climate Change as the Interaction Between Sea Ice Extent and Mean Ocean Temperature Under Orbital Insolation Forcing

  2013cites this paper
• Abrupt millennial variability and interdecadal-interstadial oscillations in a global coupled model: sensitivity to the background climate state

  2012cites this paper
• Synchronization of polar climate variability over the last ice age: in search of simple rules at the heart of climate's complexity

  2012cites this paper
• Dynamics of the British Ice Sheet and prevailing hydrographic conditions for the last 175,000 years : an investigation of marine sediment core MD04-2822 from the Rockall Trough

  2011cites this paper
• Abrupt millennial variability and interdecadal-interstadial oscillations in a global coupled model: sensitivity to the background climate state

  2011cites this paper
• Weak oceanic heat transport as a cause of the instability of glacial climates

  2010cites this paper
• An inverse model study of abrupt climate change during last ice age

  2010cites this paper
• The Role of Oceanic Heat Transport and Wind Stress Forcing in Abrupt Millennial-Scale Climate Transitions

  2010influential citation
• A New Analytical Model for Heinrich Events and Climate Instability

  2008cites this paper
• A Simple Model of Millennial Oscillations of the Thermohaline Circulation

  2007cites this paper
• Cooperative Institute for Climate Science

  2006cites this paper
• Radiation Importance Ocean Science Discussions Technical Note: Is Radiation Important for the High Amplitude Variability of the Moc in the North Atlantic? Osd Radiation Importance

  year unknowncites this paper