scholarly article | Q13442814 |
P819 | ADS bibcode | 2014GeoRL..41.6252Z |
P356 | DOI | 10.1002/2014GL060891 |
P50 | author | Ian Eisenman | Q56420582 |
Jiang Zhu | Q57164865 | ||
Zhengyu Liu | Q75719988 | ||
Wei Liu | Q97424727 | ||
P2093 | author name string | Xu Zhang | |
P2860 | cites work | The 100,000-year ice-Age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity | Q28138776 |
Variations in the Earth's Orbit: Pacemaker of the Ice Ages | Q28245451 | ||
GLOBAL GLACIAL ISOSTASY AND THE SURFACE OF THE ICE-AGE EARTH: The ICE-5G (VM2) Model and GRACE | Q30048617 | ||
The role of the thermohaline circulation in abrupt climate change | Q30675841 | ||
Abrupt glacial climate shifts controlled by ice sheet changes | Q30842427 | ||
Ocean circulation and climate during the past 120,000 years | Q34149223 | ||
Collapse and rapid resumption of Atlantic meridional circulation linked to deglacial climate changes | Q34315674 | ||
Northern Hemisphere forcing of Southern Hemisphere climate during the last deglaciation | Q39121552 | ||
Transient simulation of last deglaciation with a new mechanism for Bolling-Allerod warming | Q41995144 | ||
Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation | Q47211837 | ||
Massive iceberg discharges as triggers for global climate change | Q55933267 | ||
Rain driven by receding ice sheets as a cause of past climate change | Q56092775 | ||
Northern Hemisphere Ice-Sheet Influences on Global Climate Change | Q56553648 | ||
Bifurcations of the Atlantic thermohaline circulation in response to changes in the hydrological cycle | Q56812835 | ||
On the stability of the Atlantic meridional overturning circulation during the last deglaciation | Q57438279 | ||
The thermal threshold of the Atlantic meridional overturning circulation and its control by wind stress forcing during glacial climate | Q58072157 | ||
Last Glacial Maximum ocean thermohaline circulation: PMIP2 model intercomparisons and data constraints | Q58072222 | ||
The influence of continental ice sheets on the climate of an ice age | Q58073130 | ||
Different ocean states and transient characteristics in Last Glacial Maximum simulations and implications for deglaciation | Q58080838 | ||
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 period | Q58306246 | ||
P433 | issue | 17 | |
P407 | language of work or name | English | Q1860 |
P921 | main subject | Atlantic meridional overturning circulation | Q4652675 |
P1104 | number of pages | 7 | |
P304 | page(s) | 6252-6258 | |
P577 | publication date | 2014-09-03 | |
P1433 | published in | Geophysical Research Letters | Q5535576 |
P1476 | title | Linear weakening of the AMOC in response to receding glacial ice sheets in CCSM3 | |
P478 | volume | 41 |
Q37031048 | Correlation and anti-correlation of the East Asian summer and winter monsoons during the last 21,000 years. |
Q37515043 | Deglacial temperature history of West Antarctica |
Q58055777 | Improving the Representation of Polar Snow and Firn in the Community Earth System Model |
Q29029939 | Response of Atlantic overturning to future warming in a coupled atmosphere-ocean-ice sheet model |
Q50199716 | Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography. |
Q52565498 | Warm summers during the Younger Dryas cold reversal. |
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