In this paper, we examine the nature of the Pliocene Antarctic Peninsula Ice Sheet by comparing the terrestrial and marine geological records of the Antarctic Peninsula and surrounding sea floor with estimated net snow accumulation in the region derived from numerical palaeoclimate model experiments. Pliocene geological data and our new modelling results are consistent and mutually supportive in suggesting that an ice sheet was present even during the warmest episodes of the Pliocene. The combined results suggest that the ice sheet in the Antarctic Peninsula is more robust to globally warmer conditions than is generally assumed, at least up to the climatic limits examined in our study. Crown Copyright (C) 2009 Published by Elsevier B.V. All...
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global ...
The stability of the Earth's major ice sheets is a critical uncertainty in predictions of future cli...
This study focuses on the interactions between climate and ice sheets in order to obtain a better un...
Significant controversy exists surrounding the nature of the Antarctic ice sheet during the period o...
The mid-Pliocene warm period provides a natural laboratory to investigate the long-term response of ...
The Pliocene (c. 5.3 - 1.8 Myr BP) was the last epoch of geological time in which global temperature...
In the context of future climate change, understanding the nature and behaviour of ice sheets during...
In the context of future climate change, understanding the nature and behaviour of ice sheets during...
The mid-Pliocene warm period provides a natural laboratory to investigate the long-term response of ...
The Antarctic Peninsula region is currently undergoing rapid environmental change, resulting in the ...
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global ...
Geological evidence shows that the ice sheet and climate in Antarctica has changed considerably sinc...
The Antarctic Peninsula region is currently undergoing rapid environmental change, resulting in the ...
The climate record of glacially transported sediments in prograded wedges around the Antarctic outer...
Approximately five million years ago, during the early Pliocene, global temperatures were 2 – 4 ⁰C w...
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global ...
The stability of the Earth's major ice sheets is a critical uncertainty in predictions of future cli...
This study focuses on the interactions between climate and ice sheets in order to obtain a better un...
Significant controversy exists surrounding the nature of the Antarctic ice sheet during the period o...
The mid-Pliocene warm period provides a natural laboratory to investigate the long-term response of ...
The Pliocene (c. 5.3 - 1.8 Myr BP) was the last epoch of geological time in which global temperature...
In the context of future climate change, understanding the nature and behaviour of ice sheets during...
In the context of future climate change, understanding the nature and behaviour of ice sheets during...
The mid-Pliocene warm period provides a natural laboratory to investigate the long-term response of ...
The Antarctic Peninsula region is currently undergoing rapid environmental change, resulting in the ...
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global ...
Geological evidence shows that the ice sheet and climate in Antarctica has changed considerably sinc...
The Antarctic Peninsula region is currently undergoing rapid environmental change, resulting in the ...
The climate record of glacially transported sediments in prograded wedges around the Antarctic outer...
Approximately five million years ago, during the early Pliocene, global temperatures were 2 – 4 ⁰C w...
Warm intervals within the Pliocene epoch (5.33-2.58 million years ago) were characterized by global ...
The stability of the Earth's major ice sheets is a critical uncertainty in predictions of future cli...
This study focuses on the interactions between climate and ice sheets in order to obtain a better un...