Glacial isostatic adjustment in the static gravity field of Fennoscandia
, 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.
Novak, P. (author) +9 more
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, 2019 The SEAMIS database (Mendeley data repository; https://doi.org/10.17632/wp4ctb4667.1) contains 546 relative sea-level indicators from 31 different studies within the broader Southeast Asian region including the Maldives, India and Sri Lanka.
Stocchi P +6 more
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Glacial Isostatic Adjustment and Contemporary Sea Level Rise: An Overview
, 2017 Glacial isostatic adjustment (GIA) encompasses a suite of geophysical phenomena accompanying the waxing and waning of continental-scale ice sheets. These involve the solid Earth, the oceans and the cryosphere both on short (decade to century) and on long
SPADA, GIORGIO
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Statistical analysis of the acceleration of Baltic mean sea-level rise, 1900-2012
Frontiers in Marine Science, 2016 We analyse annual mean sea-level records from tide-gauges located in the Baltic and parts of the North Sea with the aim of detecting an acceleration of sea-level rise over the 20textsuperscript{th} and 21textsuperscript{st} centuries.
Birgit Hünicke, Eduardo Zorita
doaj +1 more source
Impact of glacial isostatic adjustment on cosmogenic surface-exposure dating
Quaternary Science Reviews, 2019 Calculating cosmogenic-nuclide surface-exposure ages is critically dependent on a knowledge of the altitude of the sample site. Changes in altitude have occurred through time as a result of glacial isostatic adjustment (GIA), potentially altering local nuclide production rates and, therefore, surface-exposure ages.
R.S. Jones +4 more
openaire +3 more sources
A simple physical model for glacial cycles [PDF]
Earth System DynamicsGlacial cycles are the norm in Pleistocene climate variability. Models of varying degree of complexity have been used to answer the question of what causes the nonlinear response of the climate system to the periodic forcing from the Sun.
S. Pérez-Montero +8 more
doaj +1 more source
Effects of Andrade and Burgers rheologies on glacial isostatic adjustment modeling in Antarctica
Geodesy and GeodynamicsVariations in ice mass deform the Earth and modify its gravity field, a process known as Glacial Isostatic Adjustment (GIA). GIA in Antarctica remains poorly constrained due to the cumulative effect of past and present ice-mass changes, the unknown ...
Alexandre Boughanemi, Anthony Mémin
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Constraining Glacial Isostatic Adjustment with Horizontal GPS Velocities in Antarctica
, 2017 Glacial isostatic adjustment is the viscoelastic response of the Earth to ice and ocean loads. In forward models of glacial isostatic adjustment, mantle viscosity is often assumed to be laterally homogeneous.
Hermans, Tim (author)
core
Uncertainty in GRACE/GRACE-follow on global ocean mass change estimates due to mis-modeled glacial isostatic adjustment and geocenter motion. [PDF]
Sci Rep, 2022 Kim JS, Seo KW, Chen J, Wilson C.
europepmc +1 more source
(Figure 8) Misfit between observations and models for the elevation of the mid-Pliocene shoreline
, 2015 RSL = relative sea level.GIA = glacial isostatic ...
Rovere, Alessio +15 more
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