Results 171 to 180 of about 653,410 (210)

Southern Ocean influence on Atlantic Meridional Overturning Circulation across climate states. [PDF]

Nat Commun
Song Z, Latif M, Park W, Zhang Y.
europepmc   +1 more source

Rate-induced tipping in marine-based regions of the Antarctic ice sheet

Swierczek-Jereczek J, Blasco J, Robinson A, Alvarez-Solas J, Montoya M.   +4 more
europepmc   +1 more source

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Modelling the glacial isostatic adjustment of the UK region

Philosophical Transactions Series A, Mathematical, Physical, and Engineering Sciences, 2006
The glacial isostatic adjustment of the UK region has been considered in a number of recent studies. We have revisited this problem in order to: (i) highlight some key issues with regard to limitations in the ice modelling approach adopted in these studies and (ii) consider the constraints provided from observations of crustal motion available via ...
Felicia Norma Teferle, Richard Bingley, G A Milne   +2 more
exaly   +4 more sources

Glacial isostatic adjustment in Fennoscandia—A review of data and modeling

Journal of Geodynamics, 2011
Abstract Fennoscandia is the key area for glacial isostatic adjustment (GIA) research. Owing to its long settlement and excellent infrastructure, ongoing land uplift in the north as well as subsidence in the south have affected human life and already triggered scientific investigations starting in the late 17th century.
Patrick Wu, Holger Steffen
exaly   +5 more sources

An improved glacial isostatic adjustment model for the British Isles

Journal of Quaternary Science, 2011
AbstractThe glacial isostatic adjustment (GIA) of the British Isles is of interest due to the constraints that can be provided on key model parameters such as the global meltwater signal, local ice sheet history and viscoelastic earth structure. A number of recent studies have modelled relative sea‐level (RSL) data from this region to constrain model ...
Glenn Milne, Robin J Edwards, Ian Shennan   +2 more
exaly   +2 more sources

Glacial isostatic adjustment: physical models and observational constraints

Reports on Progress in Physics, 2022
Abstract By far the most prescient insights into the interior structure of the planet have been provided on the basis of elastic wave seismology. Analysis of the travel times of shear or compression wave phases excited by individual earthquakes, or through analysis of the elastic gravitational free oscillations that individual ...
W Richard Peltier, Patrick Pak-Cheuk Wu, Donald F Argus, Tanghua Li, Jesse Velay-Vitow   +4 more
openaire   +3 more sources

Glacial isostatic adjustment in the static gravity field of Fennoscandia

Journal of Geophysical Research: Solid Earth, 2015
In the central part of Fennoscandia, the crust is currently rising, because of the delayed response of the viscous mantle to melting of the Late Pleistocene ice sheet.
Pavel Novak, Joerg Ebbing, Wouter van der Wal   +2 more
exaly   +3 more sources

Glacial isostatic adjustment and mantle viscosity

Journal of Geophysical Research: Solid Earth, 1988
The determination of mantle viscosity conditions from observations of relative sea level changes associated with glacial unloading of the Laurentide and Fennoscandia ice sheets has been reexamined. The conclusion is reached that the adjustment has been an upper mantle process associated with the low‐seismic‐velocity, low‐viscosity asthenospheric layer ...
Charles B. Officer, Walter S. Newman, John M. Sullivan, Daniel R. Lynch   +3 more
openaire   +1 more source

Glacial Isostatic Adjustment

Abstract
Giorgio Spada, Daniele Melini
openaire   +3 more sources