This study evaluates the influence of plausible changes in East Antarctic Ice sheet (EAIS) thickness and the subsequent glacio-isostatic response as a contributor to the Antarctic warming indicated by ice core records during the Last Interglacial period (LIG). These higher temperatures have been estimated primarily using the difference in the δD peak (on average ~ 15‰) in these LIG records relative to records for the Present Interglacial (PIG). Using a preliminary exploratory modelling study, it is shown that introducing a relatively moderate reduction in the amount of thickening of the EAIS over the LIG period introduces a significant increase (up to 8‰) in the predicted elevation-driven only δD signal at the central Antarctic Ice sheet (A...
The response of the East Antarctic Ice Sheet to global warming represents a major source of uncertai...
Constraining the stability of the East Antarctic Ice Sheet (EAIS) over glacial-interglacial timescal...
Stable isotope ratios of oxygen and hydrogen in the Antarctic ice core record have revolutionized ou...
This study evaluates the influence of plausible changes in East Antarctic Ice sheet (EAIS) thickness...
Changes of the topography of the Antarctic ice sheet (AIS) can complicate the interpretation of ice ...
Changes of the topography of the Antarctic ice sheet (AIS) can complicate the interpretation of ice ...
Studying the response of the Antarctic ice sheets during periods when climate conditions were simila...
We compare the present and last interglacial periods as recorded in Antarctic water stable isotope r...
Understanding ice sheet behaviour in the geological past is essential for evaluating the role of the...
Abundant indirect evidence suggests that the West Antarctic Ice Sheet (WAIS) reduced in size during ...
The response of the East Antarctic Ice Sheet to global warming represents a major source of uncertai...
We compare the present and last interglacial periods as recorded in Antarctic water stable isotope r...
The response of the East Antarctic Ice Sheet to global warming represents a major source of uncertai...
Constraining the stability of the East Antarctic Ice Sheet (EAIS) over glacial-interglacial timescal...
Stable isotope ratios of oxygen and hydrogen in the Antarctic ice core record have revolutionized ou...
This study evaluates the influence of plausible changes in East Antarctic Ice sheet (EAIS) thickness...
Changes of the topography of the Antarctic ice sheet (AIS) can complicate the interpretation of ice ...
Changes of the topography of the Antarctic ice sheet (AIS) can complicate the interpretation of ice ...
Studying the response of the Antarctic ice sheets during periods when climate conditions were simila...
We compare the present and last interglacial periods as recorded in Antarctic water stable isotope r...
Understanding ice sheet behaviour in the geological past is essential for evaluating the role of the...
Abundant indirect evidence suggests that the West Antarctic Ice Sheet (WAIS) reduced in size during ...
The response of the East Antarctic Ice Sheet to global warming represents a major source of uncertai...
We compare the present and last interglacial periods as recorded in Antarctic water stable isotope r...
The response of the East Antarctic Ice Sheet to global warming represents a major source of uncertai...
Constraining the stability of the East Antarctic Ice Sheet (EAIS) over glacial-interglacial timescal...
Stable isotope ratios of oxygen and hydrogen in the Antarctic ice core record have revolutionized ou...