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Erschienen in:
Perpectives on Integrated Solid Earth Sciences Kapitel lesen Erstes Kapitel lesen

2010 | OriginalPaper | Buchkapitel

DynaQlim – Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas

verfasst von : Markku Poutanen, Doris Dransch, Søren Gregersen, Sören Haubrock, Erik R. Ivins, Volker Klemann, Elena Kozlovskaya, Ilmo Kukkonen, Björn Lund, Juha-Pekka Lunkka, Glenn Milne, Jürgen Müller, Christophe Pascal, Bjørn R. Pettersen, Hans-Georg Scherneck, Holger Steffen, Bert Vermeersen, Detlef Wolf

Erschienen in: New Frontiers in Integrated Solid Earth Sciences

Verlag: Springer Netherlands

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Abstract

The isostatic adjustment of the solid Earth to the glacial loading (GIA, Glacial Isostatic Adjustment) with its temporal signature offers a great opportunity to retrieve information of Earth’s upper mantle to the changing mass of glaciers and ice sheets, which in turn is driven by variations in Quaternary climate. DynaQlim (Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas) has its focus to study the relations between upper mantle dynamics, its composition and physical properties, temperature, rheology, and Quaternary climate. Its regional focus lies on the cratonic areas of northern Canada and Scandinavia.
Geodetic methods like repeated precise levelling, tide gauges, high-resolution observations of recent movements, gravity change and monitoring of postglacial faults have given information on the GIA process for more than 100 years. They are accompanied by more recent techniques like GPS observations and the GRACE and GOCE satellite missions which provide additional global and regional constraints on the gravity field. Combining geodetic observations with seismological investigations, studies of the postglacial faults and continuum mechanical modelling of GIA, DynaQlim offers new insights into properties of the lithosphere. Another step toward a better understanding of GIA has been the joint inversion of different types of observational data – preferentially connected with geological relative sea-level evidence of the Earth’s rebound during the last 10,000 years.
Due to the changes in the lithospheric stress state large faults ruptured violently at the end of the last glaciation in large earthquakes, up to the magnitudes MW = 7–8. Whether the rebound stress is still able to trigger a significant fraction of intraplate seismic events in these regions is not completely understood due to the complexity and spatial heterogeneity of the regional stress field. Understanding of this mechanism is of societal importance.
Glacial ice sheet dynamics are constrained by the coupled process of the deformation of the viscoelastic solid Earth, the ocean and climate variability. Exactly how the climate and oceans reorganize to sustain growth of ice sheets that ground to continents and shallow continental shelves is poorly understood. Incorporation of nonlinear feedback in modelling both ocean heat transport systems and atmospheric CO2 is a major challenge. Climate-related loading cycles and episodes are expected to be important, hence also more short-term features of palaeoclimate should be explicitly treated.

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Metadaten
Titel
DynaQlim – Upper Mantle Dynamics and Quaternary Climate in Cratonic Areas
verfasst von
Markku Poutanen
Doris Dransch
Søren Gregersen
Sören Haubrock
Erik R. Ivins
Volker Klemann
Elena Kozlovskaya
Ilmo Kukkonen
Björn Lund
Juha-Pekka Lunkka
Glenn Milne
Jürgen Müller
Christophe Pascal
Bjørn R. Pettersen
Hans-Georg Scherneck
Holger Steffen
Bert Vermeersen
Detlef Wolf
Copyright-Jahr
2010
Verlag
Springer Netherlands
Buch
New Frontiers in Integrated Solid Earth Sciences

Print ISBN: 978-90-481-2736-8

Electronic ISBN: 978-90-481-2737-5

Copyright-Jahr: 2010

DOI
https://doi.org/10.1007/978-90-481-2737-5_10