Results 51 to 60 of about 8,101 (169)

The effect of sediment loading in Fennoscandia and the Barents Sea during the last glacial cycle on glacial isostatic adjustment observations [PDF]

open access: yesSolid Earth, 2017
Models for glacial isostatic adjustment (GIA) routinely include the effects of meltwater redistribution and changes in topography and coastlines. Since the sediment transport related to the dynamics of ice sheets may be comparable to that of sea level
W. van der Wal, T. IJpelaar
doaj   +1 more source

Large-scale features of Pliocene climate: results from the Pliocene Model Intercomparison Project [PDF]

open access: yes, 2013
Climate and environments of the mid-Pliocene warm period (3.264 to 3.025 Ma) have been extensively studied. Whilst numerical models have shed light on the nature of climate at the time, uncertainties in their predictions have not been systematically ...
Abe-Ouchi, Ayako   +45 more
core   +6 more sources

Timescales of glacial isostatic adjustment in Greenland: is transient rheology required?

open access: yesGeophysical Journal International
SUMMARY The possibility of a transient rheological response to ice age loading, first discussed in the literature of the 1980s, has received renewed attention. Transient behaviour across centennial to millennial timescales has been invoked to reconcile apparently contradictory inferences of steady-state (Maxwell) viscosity based on two ...
Linda Pan   +4 more
openaire   +1 more source

Countrywide Observations of Plate Spreading and Glacial Isostatic Adjustment in Iceland Inferred by Sentinel‐1 Radar Interferometry, 2015–2018

open access: yesGeophysical Research Letters, 2019
East‐west and vertical ground velocities for 2015–2018 are retrieved over 81% of Iceland from Sentinel‐1 radar interferometry, using satellite images from six different tracks. Only summertime images are considered, to avoid snow cover.
Vincent Drouin, Freysteinn Sigmundsson
doaj   +1 more source

Coeval brittle and ductile deformation beneath the late Wisconsinan Puget Lobe, Washington State, USA

open access: yesAnnals of Glaciology, 2019
Late Wisconsinan glacial sediments, exposed on Whidbey Island and Camano Island, Puget Sound (Washington State, USA), were deposited in a proglacial shallow marine/outwash environment during northward retreat of the Puget Lobe of the Cordilleran ice ...
Jasper Knight
doaj   +1 more source

Subglacial deformation and till formation in a stratigraphic complex Late Pleistocene sequence (Einödgraben/Aurach, Kitzbühel Alps, Austria) [PDF]

open access: yesEiszeitalter und Gegenwart
Knowledge of subglacial conditions is of great relevance in understanding glacier dynamics. A combination of micro- and macrosedimentological analysis of diamictons and deformation structures can form the basis for the reconstruction of past subglacial ...
J. M. Reitner, J. Menzies
doaj   +1 more source

The effects of rheological layering on post-seismic deformation [PDF]

open access: yes, 2006
We examine the effects of rheological layering on post-seismic deformation using models of an elastic layer over a viscoelastic layer and a viscoelastic half-space. We extend a general linear viscoelastic theory we have previously proposed to models with
Hager, B. H., Hetland, E. A.
core   +1 more source

Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites [PDF]

open access: yes, 2013
Late Paleozoic glacial diamictites occur in many localities in western Argentina, indicating that the region was strongly affected by glaciation during the mid-Carboniferous (late Serpukhovian–early Bashkirian).
Gulbranson, Erik L.   +6 more
core   +1 more source

Improvements on the discretisation of boundary conditions to the momentum balance for glacial ice

open access: yesJournal of Glaciology
The flow of glacial ice is typically approximated as a nonNewtonian viscous fluid, with the momentum balance described by (an approximation to) the Stokes equations, and the nonlinear rheology described by a flow law.
Constantijn J. Berends   +2 more
doaj   +1 more source

Glacial Isostatic Adjustment (GIA) in Greenland: A Review [PDF]

open access: yes, 2016
Using the most recently published regional and global deglaciation histories we provide updated estimates of the Glacial Isostatic Adjustment (GIA) component of present day uplift at a suite of GPS sites in Greenland.
Bevis, Mike   +2 more
core   +1 more source

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