Antarctic Ice Sheet change during the last glacial cycle is unclear. The timing of moraine development in the Ross basin suggests that the ice sheet reached maximum thickness under the warming temperatures of the last termination
International audienceThe East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Ear...
Reconstructing past grounding-line evolution can help inform future sea level projections by constra...
Constraining the timing of the retreat of the Last Glacial Maximum (LGM) Antarctic Ice Sheet in the ...
The Antarctic Ice Sheet contains ~58 m of global sea-level equivalent and thus its future behavior u...
Emerging ice-sheet modeling suggests once initiated, retreat of the Antarctic Ice Sheet (AIS) can co...
Reconstructing the former dimensions and deglacial history of the Antarctic Ice Sheet along with Ant...
The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting it...
An understanding of how the Antarctic ice sheet has reacted to natural global warming since the last...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting it...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
The Antarctic Ice Sheet (AIS) plays a major role in the evolution of Quaternary glacial interglacial...
The Antarctic Ice Sheet (AIS) plays a major role in the evolution of Quaternary glacial interglacial...
International audienceThe East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Ear...
International audienceThe East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Ear...
Reconstructing past grounding-line evolution can help inform future sea level projections by constra...
Constraining the timing of the retreat of the Last Glacial Maximum (LGM) Antarctic Ice Sheet in the ...
The Antarctic Ice Sheet contains ~58 m of global sea-level equivalent and thus its future behavior u...
Emerging ice-sheet modeling suggests once initiated, retreat of the Antarctic Ice Sheet (AIS) can co...
Reconstructing the former dimensions and deglacial history of the Antarctic Ice Sheet along with Ant...
The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting it...
An understanding of how the Antarctic ice sheet has reacted to natural global warming since the last...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
Retreat of the Antarctic ice sheets since the Last Glacial Maximum (LGM) has been associated with se...
The East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Earth, and documenting it...
The Antarctic Ice Sheets responded significantly to climatic conditions during the Last Glacial Maxi...
The Antarctic Ice Sheet (AIS) plays a major role in the evolution of Quaternary glacial interglacial...
The Antarctic Ice Sheet (AIS) plays a major role in the evolution of Quaternary glacial interglacial...
International audienceThe East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Ear...
International audienceThe East Antarctic Ice Sheet (EAIS) is the largest continental ice mass on Ear...
Reconstructing past grounding-line evolution can help inform future sea level projections by constra...
Constraining the timing of the retreat of the Last Glacial Maximum (LGM) Antarctic Ice Sheet in the ...