A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation

While there has been a colossal effort in the ongoing decades, the ability to simulate ocean ice has fallen behind various parts of the climate system and most Earth System Models are unable to capture the observed adversities of Arctic sea ice, which is, as it were, attributed to our frailty to det...

Full description

Bibliographic Details
Main Author: Alam, Fahim
Other Authors: Khouider, Boualem
Format: Thesis
Language:English
Published: 2023
Subjects:
Online Access:http://hdl.handle.net/1828/15217
_version_ 1821843767268737024
author Alam, Fahim
author2 Khouider, Boualem
author_facet Alam, Fahim
author_sort Alam, Fahim
collection University of Victoria (Canada): UVicDSpace
description While there has been a colossal effort in the ongoing decades, the ability to simulate ocean ice has fallen behind various parts of the climate system and most Earth System Models are unable to capture the observed adversities of Arctic sea ice, which is, as it were, attributed to our frailty to determine sea ice dynamics. Viscous Plastic rheology is the most by and large recognized model for sea ice dynamics and it is expressed as a set of partial differential equations that are hard to tackle numerically. Using the 1D sea ice momentum equation as a prototype, we use the method of lines based on Euler's backward method. This results in a nonlinear PDE in space only. At that point, we apply the Damped Newton’s method which has been introduced in Looper and Rapetti et al. and used and generalized to 2D in Saumier et al. to solve the Monge-Ampere equation. However, in our case, we need to solve 2nd order linear equation with discontinuous coefficients during Newton iteration. To overcome this difficulty, we use the Finite element method to solve the linear PDE at each Newton iteration. In this paper, we show that with the adequate smoothing and re-scaling of the linear equation, convergence can be guaranteed and the numerical solution indeed converges efficiently to the continuum solution unlike other numerical approaches that typically solve an alternate set of equations and avoid the difficulty of the Newton method for a large nonlinear algebraic system. The finite element solver failed to converge when the original setting of the smoothed SIME with a smoothing constant $K=2.8 \times 10^8$ was used. A much smaller constant of K=100 was necessary. The large smoothing constant K leads to an ill conditioned mass matrix. Graduate
format Thesis
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
geographic Arctic
Monge
geographic_facet Arctic
Monge
id ftuvicpubl:oai:dspace.library.uvic.ca:1828/15217
institution Open Polar
language English
long_lat ENVELOPE(141.482,141.482,-66.787,-66.787)
op_collection_id ftuvicpubl
op_relation http://hdl.handle.net/1828/15217
op_rights Available to the World Wide Web
publishDate 2023
record_format openpolar
spelling ftuvicpubl:oai:dspace.library.uvic.ca:1828/15217 2025-01-16T20:48:44+00:00 A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation Alam, Fahim Khouider, Boualem 2023 application/pdf http://hdl.handle.net/1828/15217 English en eng http://hdl.handle.net/1828/15217 Available to the World Wide Web SIME Newton method FEM Nonlinear PDE Numerical Method Thesis 2023 ftuvicpubl 2023-07-25T23:46:22Z While there has been a colossal effort in the ongoing decades, the ability to simulate ocean ice has fallen behind various parts of the climate system and most Earth System Models are unable to capture the observed adversities of Arctic sea ice, which is, as it were, attributed to our frailty to determine sea ice dynamics. Viscous Plastic rheology is the most by and large recognized model for sea ice dynamics and it is expressed as a set of partial differential equations that are hard to tackle numerically. Using the 1D sea ice momentum equation as a prototype, we use the method of lines based on Euler's backward method. This results in a nonlinear PDE in space only. At that point, we apply the Damped Newton’s method which has been introduced in Looper and Rapetti et al. and used and generalized to 2D in Saumier et al. to solve the Monge-Ampere equation. However, in our case, we need to solve 2nd order linear equation with discontinuous coefficients during Newton iteration. To overcome this difficulty, we use the Finite element method to solve the linear PDE at each Newton iteration. In this paper, we show that with the adequate smoothing and re-scaling of the linear equation, convergence can be guaranteed and the numerical solution indeed converges efficiently to the continuum solution unlike other numerical approaches that typically solve an alternate set of equations and avoid the difficulty of the Newton method for a large nonlinear algebraic system. The finite element solver failed to converge when the original setting of the smoothed SIME with a smoothing constant $K=2.8 \times 10^8$ was used. A much smaller constant of K=100 was necessary. The large smoothing constant K leads to an ill conditioned mass matrix. Graduate Thesis Arctic Sea ice University of Victoria (Canada): UVicDSpace Arctic Monge ENVELOPE(141.482,141.482,-66.787,-66.787)
spellingShingle SIME
Newton method
FEM
Nonlinear PDE
Numerical Method
Alam, Fahim
A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title_full A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title_fullStr A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title_full_unstemmed A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title_short A new numerical approach to solve 1D Viscous Plastic Sea Ice Momentum Equation
title_sort new numerical approach to solve 1d viscous plastic sea ice momentum equation
topic SIME
Newton method
FEM
Nonlinear PDE
Numerical Method
topic_facet SIME
Newton method
FEM
Nonlinear PDE
Numerical Method
url http://hdl.handle.net/1828/15217