Glacial isostatic adjustment modelling: historical perspectives, recent advances, and future directions
PL Whitehouse - Earth surface dynamics, 2018 - esurf.copernicus.org
Glacial isostatic adjustment (GIA) describes the response of the solid Earth, the gravitational
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
field, and the oceans to the growth and decay of the global ice sheets. A commonly studied …
Holocene relative sea-level changes from near-, intermediate-, and far-field locations
Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …
mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic …
A new global ice sheet reconstruction for the past 80 000 years
The evolution of past global ice sheets is highly uncertain. One example is the missing ice
problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present)–an …
problem during the Last Glacial Maximum (LGM, 26 000-19 000 years before present)–an …
The nature of the lithosphere‐asthenosphere boundary
Plate tectonic theory was developed 50 years ago and underpins most of our understanding
of Earth's evolution. The theory explains observations of magnetic lineations on the seafloor …
of Earth's evolution. The theory explains observations of magnetic lineations on the seafloor …
Pacific subduction control on Asian continental deformation including Tibetan extension and eastward extrusion tectonics
Abstract The India-Asia collision has formed the highest mountains on Earth and is thought
to account for extensive intraplate deformation in Asia. The prevailing explanation considers …
to account for extensive intraplate deformation in Asia. The prevailing explanation considers …
The North American Late Wisconsin ice sheet and mantle viscosity from glacial rebound analyses
K Lambeck, A Purcell, S Zhao - Quaternary Science Reviews, 2017 - Elsevier
Observations of sea level and crustal response to glacial loading cycles provide constraints
on the mantle rheology function, E, and as well as on the ice load, I, with the latter being …
on the mantle rheology function, E, and as well as on the ice load, I, with the latter being …
Regional variations in relative sea-level changes influenced by nonlinear vertical land motion
Vertical land movements can cause regional relative sea-level changes to differ
substantially from climate-driven absolute sea-level changes. Whereas absolute sea level …
substantially from climate-driven absolute sea-level changes. Whereas absolute sea level …
Post-glacial sea-level change along the Pacific coast of North America
Sea-level history since the Last Glacial Maximum on the Pacific margin of North America is
complex and heterogeneous owing to regional differences in crustal deformation …
complex and heterogeneous owing to regional differences in crustal deformation …
Simultaneous estimation of global present-day water transport and glacial isostatic adjustment
X Wu, MB Heflin, H Schotman, BLA Vermeersen… - Nature …, 2010 - nature.com
Global water transport between oceans and continents during the transition from glacial to
interglacial times has been enormous. The viscoelastic solid Earth has been responding to …
interglacial times has been enormous. The viscoelastic solid Earth has been responding to …
Constraining models of postglacial rebound using space geodesy: a detailed assessment of model ICE-5G (VM2) and its relatives
DF Argus, WR Peltier - Geophysical Journal International, 2010 - academic.oup.com
Using global positioning system, very long baseline interferometry, satellite laser ranging
and Doppler Orbitography and Radiopositioning Integrated by Satellite observations …
and Doppler Orbitography and Radiopositioning Integrated by Satellite observations …