J
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Last name: JIANG
First name: Xiuyang
International audience
Southern Europe climate oscillations at marine isotope stage 5a
International audience
Abrupt decadal-to-centennial hydroclimate changes in the Mediterranean region since the mid-Holocene
Tropical Pacific forcing on decadal-to-centennial NAO-dominated precipitation variability in northern Mediterranean over the past 6500 years
Multi-scale seasonal temperature variability and asynchronous regional hydrodynamics in Mediterranean since the middle Holocene
Stalagmite-inferred abrupt climate change in the north central Mediterranean region since 6500 years ago
A stalagmite-inferred climate record in the north central Mediterranean region since 6,500 years ago
A stalagmite-inferred climate record in the north central Mediterranean region since 6,500 years ago
A stalagmite-inferred climate record in the north central Mediterranean region since 6,500 years ago
The Weichselian glaciation is characterized by significant ocean circulation variations starting from ∼115 thousand years ago (ka) and terminating at ∼11.5 ka. The early Weichselian (115–74 ka), especially marine isotope stage (MIS) 5a at 85–74 ka, provides a window for understanding the linkage between the European westerlies and Mediterranean...
Marine isotope stage (MIS) 5a, a relatively warm period occurring 85-74 thousand years ago (ka, before AD 1950) during the last glacial, provides a window for understanding the linkage between the European westerlies and Mediterranean climate. However, lack of highly-resolved paleoclimate records with absolute chronologies hampers our knowledge...
Glacial terminations in the late Pleistocene are notable for their high rates of sea-level rise. Occurring ~340 thousand years before the present (kyr BP), Termination IV (T-IV) stands out as a significant one, during which sea-level rise rates exceeded 4 meters per century. The underlying causes of such rapid deglaciation during T-IV, however,...
Abrupt Fluctuation of northern Mediterranean hydroclimate and North Atlantic Oscillation since the middle Holocene
The Marine Isotope Stage (MIS) 11c interglacial and its preceding glacial termination represent an enigmatically intense climate response to relatively weak insolation forcing. So far, a lack of radiometric age control has confounded a detailed assessment of the insolation-climate relationship during this period. Here, we present 230 Th-dated...
Abstract The variability of the northern westerlies has been considered as one of the key elements for modern and past climate evolution. Their multiscale behavior and underlying control mechanisms, however, are incompletely understood, owing to the complex dynamics of Atlantic sea-level pressures. Here, we present a multi-annually resolved...