Vertical land motion as a key to understanding sea level change and variability
G Wöppelmann, M Marcos - Reviews of Geophysics, 2016 - Wiley Online Library
Vertical land motions are a key element in understanding how sea levels have changed
over the past century and how future sea levels may impact coastal areas. Ideally, to be …
over the past century and how future sea levels may impact coastal areas. Ideally, to be …
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 …
Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability
The marine portion of the West Antarctic Ice Sheet (WAIS) in the Amundsen Sea Embayment
(ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is …
(ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is …
GRACE, time-varying gravity, Earth system dynamics and climate change
Continuous observations of temporal variations in the Earth's gravity field have recently
become available at an unprecedented resolution of a few hundreds of kilometers. The …
become available at an unprecedented resolution of a few hundreds of kilometers. The …
Green's functions for geophysics: a review
E Pan - Reports on Progress in Physics, 2019 - iopscience.iop.org
The Green's function (GF) method, which makes use of GFs, is an important and elegant tool
for solving a given boundary-value problem for the differential equation from a real …
for solving a given boundary-value problem for the differential equation from a real …
Solid Earth change and the evolution of the Antarctic Ice Sheet
Recent studies suggest that Antarctica has the potential to contribute up to~ 15 m of sea-
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …
level rise over the next few centuries. The evolution of the Antarctic Ice Sheet is driven by a …
Glacial isostatic adjustment in Fennoscandia—a review of data and modeling
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 …
long settlement and excellent infrastructure, ongoing land uplift in the north as well as …
Geodetic measurements reveal similarities between post–Last Glacial Maximum and present-day mass loss from the Greenland ice sheet
Accurate quantification of the millennial-scale mass balance of the Greenland ice sheet
(GrIS) and its contribution to global sea-level rise remain challenging because of sparse in …
(GrIS) and its contribution to global sea-level rise remain challenging because of sparse in …
A mascon approach to assess ice sheet and glacier mass balances and their uncertainties from GRACE data
The purpose of this paper is to assess the mass changes of the Greenland Ice Sheet (GrIS),
Ice Sheets over Antarctica, and Land glaciers and Ice Caps with a global mascon method …
Ice Sheets over Antarctica, and Land glaciers and Ice Caps with a global mascon method …
[HTML][HTML] Rapid bedrock uplift in the Antarctic Peninsula explained by viscoelastic response to recent ice unloading
Since 1995 several ice shelves in the Northern Antarctic Peninsula have collapsed and
triggered ice-mass unloading, invoking a solid Earth response that has been recorded at …
triggered ice-mass unloading, invoking a solid Earth response that has been recorded at …