The role of membrane-like stresses in determining the stability and sensitivity of the Antarctic ice sheets: back pressure and grounding line motion.
about
Ice plug prevents irreversible discharge from East AntarcticaFrequency response of ice streams.Cascading lake drainage on the Greenland Ice Sheet triggered by tensile shock and fracture.Greenland supraglacial lake drainages triggered by hydrologically induced basal slip.The far reach of ice-shelf thinning in AntarcticaPresent State and Prospects of Ice Sheet and Glacier ModellingIn-situquantification of ice rheology and direct measurement of the Raymond Effect at Summit, Greenland using a phase-sensitive radarInvestigation of land ice-ocean interaction with a fully coupled ice-ocean model: 1. Model description and behaviorModeling the flow of glaciers in steep terrains: The integrated second-order shallow ice approximation (iSOSIA)Ice sheet grounding line dynamics: Steady states, stability, and hysteresis
P2860
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P2860
The role of membrane-like stresses in determining the stability and sensitivity of the Antarctic ice sheets: back pressure and grounding line motion.
description
2006 nî lūn-bûn
@nan
2006年の論文
@ja
2006年学术文章
@wuu
2006年学术文章
@zh
2006年学术文章
@zh-cn
2006年学术文章
@zh-hans
2006年学术文章
@zh-my
2006年学术文章
@zh-sg
2006年學術文章
@yue
2006年學術文章
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name
The role of membrane-like stre ...... ure and grounding line motion.
@en
The role of membrane-like stre ...... ure and grounding line motion.
@nl
type
label
The role of membrane-like stre ...... ure and grounding line motion.
@en
The role of membrane-like stre ...... ure and grounding line motion.
@nl
prefLabel
The role of membrane-like stre ...... ure and grounding line motion.
@en
The role of membrane-like stre ...... ure and grounding line motion.
@nl
P2860
P356
P1476
The role of membrane-like stre ...... ure and grounding line motion.
@en
P2860
P304
P356
10.1098/RSTA.2006.1797
P407
P577
2006-07-01T00:00:00Z