Linear weakening of the AMOC in response to receding glacial ice sheets in CCSM3

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Linear weakening of the AMOC in response to receding glacial ice sheets in CCSM3 is …
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scholarly articleQ13442814

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P819ADS bibcode2014GeoRL..41.6252Z
P356DOI10.1002/2014GL060891

P50authorIan EisenmanQ56420582
Jiang ZhuQ57164865
Zhengyu LiuQ75719988
Wei LiuQ97424727
P2093author name stringXu Zhang
P2860cites workThe 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricityQ28138776
Variations in the Earth's Orbit: Pacemaker of the Ice AgesQ28245451
GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACEQ30048617
The role of the thermohaline circulation in abrupt climate changeQ30675841
Abrupt glacial climate shifts controlled by ice sheet changesQ30842427
Ocean circulation and climate during the past 120,000 yearsQ34149223
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changesQ34315674
Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciationQ39121552
Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warmingQ41995144
Global warming preceded by increasing carbon dioxide concentrations during the last deglaciationQ47211837
Massive iceberg discharges as triggers for global climate changeQ55933267
Rain driven by receding ice sheets as a cause of past climate changeQ56092775
Northern Hemisphere Ice-Sheet Influences on Global Climate ChangeQ56553648
Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycleQ56812835
On the stability of the Atlantic meridional overturning circulation during the last deglaciationQ57438279
The thermal threshold of the Atlantic meridional overturning circulation and its control by wind stress forcing during glacial climateQ58072157
Last Glacial Maximum ocean thermohaline circulation: PMIP2 model intercomparisons and data constraintsQ58072222
The influence of continental ice sheets on the climate of an ice ageQ58073130
Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciationQ58080838
Is the wind stress forcing essential for the meridional overturning circulation?Q58090487
The key role of topography in altering North Atlantic atmospheric circulation during the last glacial periodQ58306246
P433issue17
P407language of work or nameEnglishQ1860
P921main subjectAtlantic meridional overturning circulationQ4652675
P1104number of pages7
P304page(s)6252-6258
P577publication date2014-09-03
P1433published inGeophysical Research LettersQ5535576
P1476titleLinear weakening of the AMOC in response to receding glacial ice sheets in CCSM3
P478volume41

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cites work (P2860)
Q37031048Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years.
Q37515043Deglacial temperature history of West Antarctica
Q58055777Improving the Representation of Polar Snow and Firn in the Community Earth System Model
Q29029939Response of Atlantic overturning to future warming in a coupled atmosphere-ocean-ice sheet model
Q50199716Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography.
Q52565498Warm summers during the Younger Dryas cold reversal.

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