Add to ORKGAn ice-flow model is used to simulate the Antarctic ice-sheet volume and deep-sea temperature record during Cenozoic times. We used a vertically integrated axisymmetric ice-sheet model, including bedrock adjustment. In order to overcome strong numerical hysteresis effects during climate change, the model is solved on a stretching grid. The Cenozoic reconstruction of the Antarctic ice sheet is accomplished by splitting the global oxygen isotope record derived from benthic foraminifera into an ice-volume and a deep-sea temperature component. The model is tuned to reconstruct the initiation of a large ice sheet of continental size at 34 Ma. The resulting ice volume curve shows that small ice caps
Summary Cenozoic variations of global ice volume deduced from δ18O deep-sea-core records are compare...
Sea-level records show large glacial-interglacial changes over the past million years, which on thes...
A prominent climate change of the Earth system was the onset of Antarctic glaciation near the Eocene...
An ice-flow model is used to simulate the Antarctic ice-sheet volume and deep-sea temperature record...
A simple quasi-analytical model is used to study the sensitivity of the Antarctic ice sheet to clim...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
Geological data indicate that there were major variations in Antarctic ice sheet volume and extent d...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
The oxygen isotope signal in benthic foraminifera from deep-sea cores is mainly determined by deep-o...
The extent and thickness of Antarctic sea ice have important climatic effects on radiation balance, ...
This study focuses on the interactions between climate and ice sheets in order to obtain a better un...
The ice sheet-climate model developed in this study describes the Antarctic ice sheet. It is forced ...
Ice sheet modeling results relevant to the ANDRILL project are briefly reviewed, involving West Anta...
Stable isotope records of benthic foraminifera from ODP Site 1264 in the southeastern Atlantic Ocean...
Summary Cenozoic variations of global ice volume deduced from δ18O deep-sea-core records are compare...
Sea-level records show large glacial-interglacial changes over the past million years, which on thes...
A prominent climate change of the Earth system was the onset of Antarctic glaciation near the Eocene...
An ice-flow model is used to simulate the Antarctic ice-sheet volume and deep-sea temperature record...
A simple quasi-analytical model is used to study the sensitivity of the Antarctic ice sheet to clim...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
Geological data indicate that there were major variations in Antarctic ice sheet volume and extent d...
Variations in global ice volume and temperature over the Cenozoic era have been investigated with a ...
The oxygen isotope signal in benthic foraminifera from deep-sea cores is mainly determined by deep-o...
The extent and thickness of Antarctic sea ice have important climatic effects on radiation balance, ...
This study focuses on the interactions between climate and ice sheets in order to obtain a better un...
The ice sheet-climate model developed in this study describes the Antarctic ice sheet. It is forced ...
Ice sheet modeling results relevant to the ANDRILL project are briefly reviewed, involving West Anta...
Stable isotope records of benthic foraminifera from ODP Site 1264 in the southeastern Atlantic Ocean...
Summary Cenozoic variations of global ice volume deduced from δ18O deep-sea-core records are compare...
Sea-level records show large glacial-interglacial changes over the past million years, which on thes...
A prominent climate change of the Earth system was the onset of Antarctic glaciation near the Eocene...