PARASO, a circum-Antarctic fully-coupled ice-sheet-ocean-sea-ice-atmosphere-land model involving f. ETISh1. 7, NEMO3. 6, LIM3. 6, COSMO5. 0 and CLM4. 5
C Pelletier, T Fichefet, H Goosse… - Geoscientific Model …, 2021 - gmd.copernicus.org
We introduce PARASO, a novel five-component fully-coupled regional climate model over
an Antarctic circumpolar domain covering the full Southern Ocean. The state-of-the-art …
an Antarctic circumpolar domain covering the full Southern Ocean. The state-of-the-art …
Projections of peak water timing from the East Rongbuk Glacier, Mt. Everest, using a higher‐order ice flow model
In this study, we apply a three‐dimensional (3D) thermomechanically coupled higher‐order
ice flow model to simulate the East Rongbuk Glacier (ERG), Mt. Everest. We first …
ice flow model to simulate the East Rongbuk Glacier (ERG), Mt. Everest. We first …
格陵兰冰盖监测, 模拟及气候影响研究
效存德， 陈卓奇， 江利明， 丁明虎， 窦挺峰 - 地球科学进展, 2019 - adearth.ac.cn
摘要格陵兰冰盖是地球上两大仅存冰盖之一. 随着气候变暖的加剧, 格陵兰冰盖的消融及其对海
平面上升的贡献成为国际上研究的热点问题. 格陵兰冰盖全部融化将会导致全球海平面上升约 …
平面上升的贡献成为国际上研究的热点问题. 格陵兰冰盖全部融化将会导致全球海平面上升约 …
A comparison between three-dimensional, transient, thermomechanically coupled first-order and Stokes ice flow models
In this study, we investigate the differences between two transient, three-dimensional,
thermomechanically coupled ice-sheet models, namely, a first-order approximation model …
thermomechanically coupled ice-sheet models, namely, a first-order approximation model …
[HTML][HTML] 东南极冰盖Lambert 冰川流域300 年来降雪记录
丁明虎， 肖王星， 效存德， 杨佼， 张东启， 李润祥， 张通 - 第四纪研究, 2017 - html.rhhz.net
利用中国第18 次南极考察队内陆冰盖考察队获得的102m 冰芯资料, 恢复了南极洲Lambert
冰川流域东侧地区300 年来的降雪量/雪积累率变化情况, 并使用Nye 模型和DJ 模型进行了较准 …
冰川流域东侧地区300 年来的降雪量/雪积累率变化情况, 并使用Nye 模型和DJ 模型进行了较准 …
A study of monitoring, simulation and climate impact of greenland ice sheet
X Cunde, C Zhuoqi, J Liming, D Minghu… - Advances in Earth …, 2019 - adearth.ac.cn
Greenland Ice Sheet is one of the two largest ice sheets on the planet. Under the
background of climate warming, the melting of the Greenland ice sheet and its contribution …
background of climate warming, the melting of the Greenland ice sheet and its contribution …
Assessing the benefits of approximately exact step sizes for Picard and Newton solver in simulating ice flow (FEniCS-full-Stokes v. 1.3. 2)
N Schmidt, A Humbert, T Slawig - Geoscientific Model …, 2024 - gmd.copernicus.org
Solving the momentum balance is the computationally expensive part of simulating the
evolution of ice sheets. The momentum balance is described by the nonlinear full-Stokes …
evolution of ice sheets. The momentum balance is described by the nonlinear full-Stokes …
A full Stokes subgrid scheme in two dimensions for simulation of grounding line migration in ice sheets using Elmer/ICE (v8. 3)
G Cheng, P Lötstedt… - Geoscientific Model …, 2020 - gmd.copernicus.org
The flow of large ice sheets and glaciers can be simulated by solving the full Stokes
equations using a finite element method. The simulation is particularly sensitive to the …
equations using a finite element method. The simulation is particularly sensitive to the …
[PDF][PDF] CMIP6 冰盖模式比较计划(ISMIP) 概况与评述
李腾， 程晓， 刘岩， 张通， 王兰宁， 刘骥平 - 气候变化研究进展, 2020 - climatechange.cn
冰盖是大面积(超过50000 km2) 覆盖陆地表面的极厚冰体, 在重力作用下的形变宏观上表现为由
内陆向沿海流动[1], 当前世界上仅存格陵兰和南极两大冰盖. 广大的内陆区域冰雪终年不化 …
内陆向沿海流动[1], 当前世界上仅存格陵兰和南极两大冰盖. 广大的内陆区域冰雪终年不化 …
The snowfall history of Lambert glacier basin during the past 300 years inferred from an ice core at LGB69, East Antarctica
M Ding, W Xiao, C Xiao, J Yang, D Zhang, R Li… - Quaternary …, 2017 - dsjyj.com.cn
Based on a 102m ice core drilled at LGB69 (70 50'06.6" S, 77 04'28.9" E; 1850m asl) of East
Antarctica, by 18th Chinese National Antarctic Research Expedition, we reconstructed the …
Antarctica, by 18th Chinese National Antarctic Research Expedition, we reconstructed the …