Hydrological modeling of stalagmite δ18O response to glacial-interglacial transitions

Theories and Modeling of Glacial–Interglacial Cycles and Glacial Inception

Glacial-interglacial dynamics of Antarctic firn columns

Introduction Conclusions References

Glacial-Interglacial Atmospheric CO2 Change —The Glacial Burial Hypothesis

Organic carbon buried under the great ice sheets of the Northern Hemisphere is suggested to be the missing link in the atmospheric CO2 change over the glacial-interglacial cycles. At glaciation, the advancement of continental ice sheets buries vegetation and soil carbon accumulated during warmer periods. At deglaciation, this burial carbon is released back into the atmosphere. In a simulation o...

Simulating last interglacial and glacial inception

Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Abstract Introduction Conclusions References Tables Figures ◭ ◮ ◭ ◮ Back Close Full Screen / Esc Printer-friendly Version Interactive Discussion EGU Abstract The Planet Simulator was used to perform equilibrium simulations of the Eemian inter-glacial at 125 kyBP and the glacial inception at 115 kyBP. Additio...

Vegetation response to glacial–interglacial climate variability near Lake Malawi in the southern African tropics

a r t i c l e i n f o Pollen records from Lake Malawi, Africa spanning the last 135 kyr show substantial and abrupt vegetation response to multiple episodes of extreme aridity between 135 and 75 ka. Peaks in both the relative abundance and total production of Podocarpus pollen define the first two of these drought episodes. From 135 to 127 and again from 117 to 105 kyr BP, Podocarpus percentage...