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Refinement of palaeotopography in modelling of glacial isostatic adjustment
2011When modelling the glacial-isotatic adjustment (GIA) by an initial value approach, the earth is assumed to be hydrostatically prestressed in an initial state. Including the sea-level equation in a solution requires, in addition, to define an initial topography, for which the present-day topography is mostly chosen.
Klemann, V. ; https://orcid.org/0000-0002-8342-8947 +2 more
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Geodetic constraints on glacial isostatic adjustment
2002John M. Wahr, James L. Davis
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Glacial Isostatic Adjustment Models for Earthquake Triggering
2021Patrick Wu +3 more
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Glacial isostatic adjustment – the spider in the geo-web
Glacial isostatic adjustment (GIA) is the response of the Earth to ice-mass changes associated with glacial loading and unloading. GIA affects the entire Earth system, from the surface down to the core-mantle boundary and from the poles to the equator, spanning timescales from decades to glacial-interglacial periods.openaire +1 more source
Glacial isostatic adjustment and the Earth system
2002Jerry X. Mitrovica +1 more
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Reply to comment by W. R. Peltier et al. on “Ocean mass from GRACE and glacial isostatic adjustment”
Journal of Geophysical Research, 2012Don Chambers
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Glacial Isostatic Adjustment over Antarctica from combined ICESat and GRACE satellite data
Earth and Planetary Science Letters, 2009Riccardo Riva +2 more
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Global sea level rise and glacial isostatic adjustment
Global and Planetary Change, 1999W R Peltier
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Time Variable Gravity: Glacial Isostatic Adjustment
2007J.X. Mitrovica +2 more
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