Global environmental consequences of twenty-first-century ice-sheet melt
Government policies currently commit us to surface warming of three to four degrees Celsius
above pre-industrial levels by 2100, which will lead to enhanced ice-sheet melt. Ice-sheet …
above pre-industrial levels by 2100, which will lead to enhanced ice-sheet melt. Ice-sheet …
Millennial to orbital-scale variations of drought intensity in the Eastern Mediterranean
M Stockhecke, A Timmermann, R Kipfer… - Quaternary Science …, 2016 - Elsevier
Millennial to orbital-scale rainfall changes in the Mediterranean region and corresponding
variations in vegetation patterns were the result of large-scale atmospheric reorganizations …
variations in vegetation patterns were the result of large-scale atmospheric reorganizations …
Glaciology and geological signature of the Last Glacial Maximum Antarctic ice sheet
Dynamical changes in contemporary ice sheets account for significant proportions of their
current rates of mass loss, but assessing whether or not these processes are a natural part …
current rates of mass loss, but assessing whether or not these processes are a natural part …
Quantification of Asian monsoon variability from 68 ka BP through pollen-based climate reconstruction
X Zhang, Z Zheng, K Huang, J Cheng, R Cheddadi… - Science Bulletin, 2023 - Elsevier
The glacial-interglacial variability of precipitation and its driving mechanism in monsoonal
regions has long been a subject of debate. However, there are few records of quantitative …
regions has long been a subject of debate. However, there are few records of quantitative …
Greenland temperature response to climate forcing during the last deglaciation
Greenland ice core water isotopic composition (δ18O) provides detailed evidence for abrupt
climate changes but is by itself insufficient for quantitative reconstruction of past …
climate changes but is by itself insufficient for quantitative reconstruction of past …
Abrupt glacial climate shifts controlled by ice sheet changes
During glacial periods of the Late Pleistocene, an abundance of proxy data demonstrates
the existence of large and repeated millennial-scale warming episodes, known as …
the existence of large and repeated millennial-scale warming episodes, known as …
A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting
The most rapid global sea-level rise event of the last deglaciation, Meltwater Pulse 1A (MWP-
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
1A), occurred∼ 14,650 years ago. Considerable uncertainty regarding the sources of …
Synchronous timing of abrupt climate changes during the last glacial period
Abrupt climate changes during the last glacial period have been detected in a global array of
palaeoclimate records, but our understanding of their absolute timing and regional …
palaeoclimate records, but our understanding of their absolute timing and regional …
Atmospheric circulation over Europe during the Younger Dryas
The Younger Dryas (YD) was a period of rapid climate cooling that occurred at the end of the
last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD …
last glaciation. Here, we present the first palaeoglacier-derived reconstruction of YD …
Coherent deglacial changes in western Atlantic Ocean circulation
Abrupt climate changes in the past have been attributed to variations in Atlantic Meridional
Overturning Circulation (AMOC) strength. However, the exact timing and magnitude of past …
Overturning Circulation (AMOC) strength. However, the exact timing and magnitude of past …