[HTML][HTML] Global sea-level budget and ocean-mass budget, with focus on advanced data products and uncertainty characterisation

M Horwath, BD Gutknecht, A Cazenave… - Earth System …, 2021 - essd.copernicus.org
Studies of the global sea-level budget (SLB) and the global ocean-mass budget (OMB) are
essential to assess the reliability of our knowledge of sea-level change and its contributors …

A mascon approach to assess ice sheet and glacier mass balances and their uncertainties from GRACE data

EJO Schrama, B Wouters… - Journal of Geophysical …, 2014 - Wiley Online Library
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 …

The solid Earth's influence on sea level

CP Conrad - Bulletin, 2013 - pubs.geoscienceworld.org
Because it lies at the intersection of Earth's solid, liquid, and gaseous components, sea level
links the dynamics of the fluid part of the planet with those of the solid part of the planet …

[HTML][HTML] Rapid bedrock uplift in the Antarctic Peninsula explained by viscoelastic response to recent ice unloading

GA Nield, VR Barletta, A Bordoni, MA King… - Earth and Planetary …, 2014 - Elsevier
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 …

[HTML][HTML] Effect of GIA models with 3D composite mantle viscosity on GRACE mass balance estimates for Antarctica

W van der Wal, PL Whitehouse… - Earth and Planetary …, 2015 - Elsevier
Seismic data indicate that there are large viscosity variations in the mantle beneath
Antarctica. Consideration of such variations would affect predictions of models of Glacial …

[HTML][HTML] Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM)–Part 2: parameter ensemble analysis

T Albrecht, R Winkelmann, A Levermann - The Cryosphere, 2020 - tc.copernicus.org
Abstract The Parallel Ice Sheet Model (PISM) is applied to the Antarctic Ice Sheet over the
last two glacial cycles (≈ 210 000 years) with a resolution of 16 km. An ensemble of 256 …

[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 …

Accelerated West Antarctic ice mass loss continues to outpace East Antarctic gains

C Harig, FJ Simons - Earth and Planetary Science Letters, 2015 - Elsevier
While multiple data sources have confirmed that Antarctica is losing ice at an accelerating
rate, different measurement techniques estimate the details of its geographically highly …

[HTML][HTML] Reconstruction of ice-sheet changes in the Antarctic Peninsula since the Last Glacial Maximum

CÓ Cofaigh, BJ Davies, SJ Livingstone… - Quaternary Science …, 2014 - Elsevier
This paper compiles and reviews marine and terrestrial data constraining the dimensions
and configuration of the Antarctic Peninsula Ice Sheet (APIS) from the Last Glacial Maximum …

[HTML][HTML] Glacial-cycle simulations of the Antarctic Ice Sheet with the Parallel Ice Sheet Model (PISM)–Part 1: Boundary conditions and climatic forcing

T Albrecht, R Winkelmann, A Levermann - The Cryosphere, 2020 - tc.copernicus.org
Simulations of the glacial–interglacial history of the Antarctic Ice Sheet provide insights into
dynamic threshold behavior and estimates of the ice sheet's contributions to global sea-level …