A stalagmite-inferred paleo-hydroclimate record during 79-89 thousand years ago from Monaco
The circum-Mediterranean region is the cradle of ancient civilizations that had their roots in the Holocene. Climate change has been considered a key element that contributed to their rise or fall. The Roman Warm Period (RWP), 200 B.C. to 400 A.D., was the warmest period in Europe during the last two thousand years. Hydroclimatic change at the...
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Southern Europe climate oscillations at marine isotope stage 5a
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Tropical Pacific forcing on decadal-to-centennial NAO-dominated precipitation variability in northern Mediterranean over the past 6500 years
Abrupt decadal-to-centennial hydroclimate changes in the Mediterranean region since the mid-Holocene
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
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...
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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...
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Abrupt Fluctuation of northern Mediterranean hydroclimate and North Atlantic Oscillation since the middle Holocene