The late Holocene retreat of the West Antarctic ice sheet is crucial information for assessing its current dynamics. However, data from this period for parts of the ice sheet where significant change has taken place, mainly the Ross Sea, are very sparse. Some significant dated deposits are from lakes dammed by valley glaciers, themselves dammed by the Ross Ice Sheet. The least age of these deposits is somewhat later than the retreat of the Ross Ice Sheet from the locality on account of the lagged response of the glacier. We present a model of the Hatherton Glacier, which examines its relationship to the Ross ice sheet, using dated margin data from ice-dammed lakes. Problems in modelling are the coupling with the Darwin Glacier, the unknown ...
Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine developme...
Outlet glaciers grounded on a bed that deepens inland and extends below sea level are potentially vu...
The retreat of the East Antarctic ice sheet at the end of the last glacial period has been attribute...
Chronologies of glacier deposits in the Transantarctic Mountains provide important constraints on gr...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
the Last Glacial Maximum (~20 ka), marine evidence indicates that the grounding line of the West Ant...
The extent and volume of the Antarctic ice sheet at the Last Glacial Maximum (LGM), as well as the t...
Understanding the history of the Ross Sea ice sheet bears on questions concerning the stability of t...
Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage basin can...
An understanding of how the Antarctic ice sheet has reacted to natural global warming since the last...
The Darwin-Hatherton glacial system (DHGS) drains from the East Antarctic Ice Sheet (EAIS) and throu...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
This dataset contains .mat files of model output from an isothermal, 1.5-dimensional, shallow-ice gl...
The timing of West Antarctic Ice Sheet (WAIS) expansion and retreat during the last glacial cycle is...
The timing of West Antarctic Ice Sheet (WAIS) expansion and retreat during the last glacial cycle is...
Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine developme...
Outlet glaciers grounded on a bed that deepens inland and extends below sea level are potentially vu...
The retreat of the East Antarctic ice sheet at the end of the last glacial period has been attribute...
Chronologies of glacier deposits in the Transantarctic Mountains provide important constraints on gr...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
the Last Glacial Maximum (~20 ka), marine evidence indicates that the grounding line of the West Ant...
The extent and volume of the Antarctic ice sheet at the Last Glacial Maximum (LGM), as well as the t...
Understanding the history of the Ross Sea ice sheet bears on questions concerning the stability of t...
Studying the history of ice-sheet behaviour in the Ross Sea, Antarctica's largest drainage basin can...
An understanding of how the Antarctic ice sheet has reacted to natural global warming since the last...
The Darwin-Hatherton glacial system (DHGS) drains from the East Antarctic Ice Sheet (EAIS) and throu...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
This dataset contains .mat files of model output from an isothermal, 1.5-dimensional, shallow-ice gl...
The timing of West Antarctic Ice Sheet (WAIS) expansion and retreat during the last glacial cycle is...
The timing of West Antarctic Ice Sheet (WAIS) expansion and retreat during the last glacial cycle is...
Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine developme...
Outlet glaciers grounded on a bed that deepens inland and extends below sea level are potentially vu...
The retreat of the East Antarctic ice sheet at the end of the last glacial period has been attribute...