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 …
The sensitivity of the Antarctic ice sheet to a changing climate: Past, present, and future
Abstract The Antarctic Ice Sheet (AIS) is out of equilibrium with the current anthropogenic‐
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
enhanced climate forcing. Paleoenvironmental records and ice sheet models reveal that the …
Global sea-level budget 1993-present
Global mean sea level is an integral of changes occurring in the climate system in response
to unforced climate variability as well as natural and anthropogenic forcing factors. Its …
to unforced climate variability as well as natural and anthropogenic forcing factors. Its …
GIA model statistics for GRACE hydrology, cryosphere, and ocean science
We provide a new analysis of glacial isostatic adjustment (GIA) with the goal of assembling
the model uncertainty statistics required for rigorously extracting trends in surface mass from …
the model uncertainty statistics required for rigorously extracting trends in surface mass from …
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 …
Mass balance of the ice sheets and glaciers–Progress since AR5 and challenges
Recent research shows increasing decadal ice mass losses from the Greenland and
Antarctic Ice Sheets and more generally from glaciers worldwide in the light of continued …
Antarctic Ice Sheets and more generally from glaciers worldwide in the light of continued …
[HTML][HTML] 基于GRACE RL06 数据监测和分析南极冰盖27 个流域质量变化
高春春， 陆洋， 史红岭， 张子占， 徐长仪， 谭冰 - 地球物理学报, 2019 - html.rhhz.net
本文基于CSR 最新公布的GRACE RL06 版本数据, 采用Slepian 空域反演法估算了南极冰盖27
个流域的质量变化. Slepian 空域反演法结合了Slepian 空间谱集中法和空域反演法的技术优势 …
个流域的质量变化. Slepian 空域反演法结合了Slepian 空间谱集中法和空域反演法的技术优势 …
Acceleration of dynamic ice loss in Antarctica from satellite gravimetry
The dynamic stability of the Antarctic Ice Sheet is one of the largest uncertainties in
projections of future global sea-level rise. Essential for improving projections of the ice sheet …
projections of future global sea-level rise. Essential for improving projections of the ice sheet …
An ensemble of Antarctic deglacial simulations constrained by geological observations
ML Pittard, PL Whitehouse, MJ Bentley… - Quaternary Science …, 2022 - Elsevier
The Antarctic ice sheet has the potential to make a significant contribution to future sea-level
rise. Understanding this potential and making projections of future ice sheet mass change …
rise. Understanding this potential and making projections of future ice sheet mass change …
Observational requirements for long-term monitoring of the global mean sea level and its components over the altimetry era
A Cazenave, B Hamlington, M Horwath… - Frontiers in Marine …, 2019 - frontiersin.org
Present-day global mean sea level rise is caused by ocean thermal expansion, ice mass
loss from glaciers and ice sheets, as well as changes in terrestrial water storage. For that …
loss from glaciers and ice sheets, as well as changes in terrestrial water storage. For that …