The deglacial transition from the last glacial maximum at ∼20 kiloyears before present (ka) to the Holocene (11.7 ka to Present) was interrupted by millennial-scale cold reversals, viz., Antarctic Cold Reversal (∼14.5–12.8 ka) and Greenland Younger Dryas (∼12.8–11.8 ka) which had different timings and extent of cooling in each hemisphere. The cause of this synchronously initiated, but different hemispheric cooling during these cold reversals (Antarctic Cold Reversal ∼3∘C and Younger Dryas ∼10∘C) is elusive because CO2, the fundamental forcing for deglaciation, and Atlantic meridional overturning circulation, the driver of antiphased bipolar climate response, both fail to explain this asymmetry. We use centennial-resolution records of the lo...
During the last glacial period, polar ice cores indicate climate asynchrony between the poles at the...
A detailed deuterium excess proÞle measured along the Dome C EPICA (European Project for Ice Coring ...
South Asian precipitation amount and extreme variability are predicted to increase due to thermodyna...
The deglacial transition from the last glacial maximum at ∼20 kiloyears before present (ka) to the H...
The Indian Summer Monsoon, a subsystem of the Asian Monsoon, is one of Earth’s most dynamic expressi...
International audienceSeveral paleoclimate records such as from Chinese loess, speleothems or upwell...
The responses of Asian monsoon subsystems to both hemispheric climate forcing and external orbital f...
Abstract Modulation of a monsoon under glacial forcing is examined using an atmosphere–ocean coupled...
The mechanisms driving glacial-interglacial changes in the climate of the Indo-Pacific warm pool are...
International audienceSea surface temperature and oxygen isotopic records from two well-dated Indian...
The monsoon is one of the most important climatic phenomena: it promotes inter-hemispheric exchange ...
During the last glacial period, polar ice cores indicate climate asynchrony between the poles at the...
A detailed deuterium excess proÞle measured along the Dome C EPICA (European Project for Ice Coring ...
South Asian precipitation amount and extreme variability are predicted to increase due to thermodyna...
The deglacial transition from the last glacial maximum at ∼20 kiloyears before present (ka) to the H...
The Indian Summer Monsoon, a subsystem of the Asian Monsoon, is one of Earth’s most dynamic expressi...
International audienceSeveral paleoclimate records such as from Chinese loess, speleothems or upwell...
The responses of Asian monsoon subsystems to both hemispheric climate forcing and external orbital f...
Abstract Modulation of a monsoon under glacial forcing is examined using an atmosphere–ocean coupled...
The mechanisms driving glacial-interglacial changes in the climate of the Indo-Pacific warm pool are...
International audienceSea surface temperature and oxygen isotopic records from two well-dated Indian...
The monsoon is one of the most important climatic phenomena: it promotes inter-hemispheric exchange ...
During the last glacial period, polar ice cores indicate climate asynchrony between the poles at the...
A detailed deuterium excess proÞle measured along the Dome C EPICA (European Project for Ice Coring ...
South Asian precipitation amount and extreme variability are predicted to increase due to thermodyna...