ProjectDANGER DML – Deciphering the evolution of an East ANtarctic drainage system over the last Glacial cycle in westERn…
Basic data
Acronym:
DANGER DML
Title:
Deciphering the evolution of an East ANtarctic drainage system over the last Glacial cycle in westERn Dronning Maud Land
Duration:
01/01/2023 to 31/12/2024
Abstract / short description:
An understanding of Antarctic ice-sheet behaviour is critical for
evaluating the role of the polar ice caps in the climate system and for
constraining the global impact of sea-level rise in a future warming
climate. Critical for assessing the potential future behaviour of the
East Antarctic Ice Sheet is to document how it changed over the last
glacial cycle (~ 0 – 115 thousand years ago) and to identify areas that
were vulnerable to these changes. However, there is a lack of suitable
observations and models that can realistically simulate East
Antarctica's ice-sheet evolution. This deficiency will be addressed in
DANGER DML. The overall goal of the project is to better understand
how a major sector of the East Antarctic Ice Sheet reacted to icesheet
changes during the last glacial cycle by applying a novel
structural analysis method for internal layers in the ice to reconstruct
ice-flow patterns of the past. This enables a new way to investigate
the past ice-dynamic behaviour of a major drainage basin in Dronning
Maud Land (Jutulstraumen and its neighboring catchments) over the
last glacial cycle and in particular the transition from the Last Glacial
Maximum to the Holocene.
evaluating the role of the polar ice caps in the climate system and for
constraining the global impact of sea-level rise in a future warming
climate. Critical for assessing the potential future behaviour of the
East Antarctic Ice Sheet is to document how it changed over the last
glacial cycle (~ 0 – 115 thousand years ago) and to identify areas that
were vulnerable to these changes. However, there is a lack of suitable
observations and models that can realistically simulate East
Antarctica's ice-sheet evolution. This deficiency will be addressed in
DANGER DML. The overall goal of the project is to better understand
how a major sector of the East Antarctic Ice Sheet reacted to icesheet
changes during the last glacial cycle by applying a novel
structural analysis method for internal layers in the ice to reconstruct
ice-flow patterns of the past. This enables a new way to investigate
the past ice-dynamic behaviour of a major drainage basin in Dronning
Maud Land (Jutulstraumen and its neighboring catchments) over the
last glacial cycle and in particular the transition from the Last Glacial
Maximum to the Holocene.
Keywords:
Antarctica
Antarktis
glaciers
Gletscher
geophysics
Geophysik
paleoclimate
Paläoklima
Involved staff
Managers
Faculty of Science
University of Tübingen
University of Tübingen
Mineralogy and Geodynamics Research Area
Department of Geoscience, Faculty of Science
Department of Geoscience, Faculty of Science
Local organizational units
Department of Geoscience
Faculty of Science
University of Tübingen
University of Tübingen
Funders
Bonn, Nordrhein-Westfalen, Germany
Cooperations
Stockholm, Sweden
Bern, Switzerland
Edinburgh, United Kingdom
Lawrence, Kansas, United States
Tromsø, Norway