A Global Shallow Ice Sheet Model and its Numerical Simulation

2009 ◽  
Author(s):  
N. Calvo ◽  
J. Durany ◽  
C. Vazquez
Keyword(s):  
Numerical Simulation ◽  
Ice Sheet

Numerical simulation on the breakup of an ice sheet induced by regular incident waves

2022 ◽  
Vol 120 ◽  
pp. 103024
Author(s):  
Kangjian He ◽  
Baoyu Ni ◽  
Xuesong Xu ◽  
Hongyu Wei ◽  
Yanzhuo Xue
Keyword(s):  
Numerical Simulation ◽  
Ice Sheet ◽  
Incident Waves

scholarly journals Numerical Simulation of the Evolution of Ice Covers Using the Scandinavian and Laurentide Ice Sheets as Examples

1982 ◽  
Vol 28 (99) ◽  
pp. 267-272 ◽  
Author(s):  
D. D. Kvasov ◽  
M. Ya. Verbitsky
Keyword(s):  
Differential Equation ◽  
Numerical Simulation ◽  
Ordinary Differential Equation ◽  
Mass Balance ◽  
Climate Models ◽  
Ice Sheets ◽  
Ice Sheet ◽  
Linear Parabolic Equation ◽  
Last Glaciation ◽  
Horizontal Size

AbstractA non-linear parabolic equation describing the evolution of an isothermal linearly viscous ice sheet is numerically solved in non-dimensional coordinates obtained by normalization over the horizontal size of a glacier. The horizontal size of the ice sheet is defined from the solution of an ordinary differential equation, the integral mass balance. For simple climate models, approximate relations describing the evolution of glaciers are proposed. These relations and palaeogeographical data are used to estimate changes in the mass balance on the surface of the Scandinavian and Laurentide ice sheets during retreat of the last glaciation.

Numerical Simulation of the Evolution of Ice Covers Using the Scandinavian and Laurentide Ice Sheets as Examples

1982 ◽  
Vol 28 (99) ◽  
pp. 267-272
Author(s):  
D. D. Kvasov ◽  
M. Ya. Verbitsky
Keyword(s):  
Differential Equation ◽  
Numerical Simulation ◽  
Ordinary Differential Equation ◽  
Mass Balance ◽  
Climate Models ◽  
Ice Sheets ◽  
Ice Sheet ◽  
Linear Parabolic Equation ◽  
Last Glaciation ◽  
Horizontal Size

AbstractA non-linear parabolic equation describing the evolution of an isothermal linearly viscous ice sheet is numerically solved in non-dimensional coordinates obtained by normalization over the horizontal size of a glacier. The horizontal size of the ice sheet is defined from the solution of an ordinary differential equation, the integral mass balance. For simple climate models, approximate relations describing the evolution of glaciers are proposed. These relations and palaeogeographical data are used to estimate changes in the mass balance on the surface of the Scandinavian and Laurentide ice sheets during retreat of the last glaciation.

Ice-flow patterns and dispersal of erratics at the southwestern margin of the last Scandinavian Ice Sheet: signature of palaeo-ice streams

Boreas ◽  
2003 ◽  
Vol 32 (1) ◽  
pp. 130-148 ◽  
Author(s):  
KURT H. KJÆR ◽  
MICHAEL HOUMARK-NIELSEN ◽  
NIELS RICHARDT
Keyword(s):  
Ice Sheet ◽  
Flow Patterns ◽  
Ice Streams ◽  
Ice Flow ◽  
Scandinavian Ice Sheet ◽  
Southwestern Margin

Water uptake by substituted amylose tablets: experimentation and numerical simulation

2009 ◽  
Vol 00 (00) ◽  
pp. 090904073309027-8
Author(s):  
H.W. Wang ◽  
S. Kyriacos ◽  
L. Cartilier
Keyword(s):  
Numerical Simulation ◽  
Water Uptake
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