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Implementation of a visco-plastic sea ice model into OpenFOAM

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dc.contributor.author Bogaers, Alfred EJ
dc.contributor.author Jansen van Rensburg, GJ
dc.contributor.author Marquart, R
dc.contributor.author Skatulla, S
dc.date.accessioned 2018-10-23T12:40:39Z
dc.date.available 2018-10-23T12:40:39Z
dc.date.issued 2018-09
dc.identifier.citation Bogaers, A.E.J. et al. 2018. Implementation of a visco-plastic sea ice model into OpenFOAM. Eleventh South African Conference on Computational and Applied Mechanics (SACAM 2018), Vanderbijlpark, South Africa, 17-19 September 2018 en_US
dc.identifier.uri http://hdl.handle.net/10204/10490
dc.description Paper presented at the Eleventh South African Conference on Computational and Applied Mechanics (SACAM 2018), Vanderbijlpark, South Africa, 17-19 September 2018 en_US
dc.description.abstract In this paper, we outline the implementation of Hibler’s visco-plastic (VP) sea ice model into OpenFOAM, an opensource finite-volume modelling toolkit. Hibler’s visco-plastic model is arguably the most widely used description of sea ice rheology, and finds application in most global climate models. The VP model has been shown to accurately capture the bulk behaviour of sea ice at large length scales. Under convergent conditions, the VP model allows the sea ice to deform plastically, while for small strains, near drift like conditions can be captured. Unfortunately however, due to the potential for large viscosities, the VP model tends to become numerically unstable. The general consensus in literature is that an implicit solution scheme is required, which tend to become expensive when used in global climate models. Suggestions to improve the convergence behaviour include techniques such as successive over-relaxation or via the addition of an elastic term, known as the elastic-visco-plastic (EVP) method. In this paper, we aim introduce the concept of dynamic relaxation, which in addition to matrix conditioning, can be used to both stabilise and accelerate the iterative convergence behaviour. The behaviour of the sea ice model will be demonstrated on a number of test cases. en_US
dc.language.iso en en_US
dc.relation.ispartofseries Worklist;21444
dc.subject Sea ice modelling en_US
dc.subject OpenFOAM en_US
dc.subject Visco-plastic rheology en_US
dc.subject Dynamic relaxation en_US
dc.title Implementation of a visco-plastic sea ice model into OpenFOAM en_US
dc.type Conference Presentation en_US
dc.identifier.apacitation Bogaers, A. E., Jansen van Rensburg, G., Marquart, R., & Skatulla, S. (2018). Implementation of a visco-plastic sea ice model into OpenFOAM. http://hdl.handle.net/10204/10490 en_ZA
dc.identifier.chicagocitation Bogaers, Alfred EJ, GJ Jansen van Rensburg, R Marquart, and S Skatulla. "Implementation of a visco-plastic sea ice model into OpenFOAM." (2018): http://hdl.handle.net/10204/10490 en_ZA
dc.identifier.vancouvercitation Bogaers AE, Jansen van Rensburg G, Marquart R, Skatulla S, Implementation of a visco-plastic sea ice model into OpenFOAM; 2018. http://hdl.handle.net/10204/10490 . en_ZA
dc.identifier.ris TY - Conference Presentation AU - Bogaers, Alfred EJ AU - Jansen van Rensburg, GJ AU - Marquart, R AU - Skatulla, S AB - In this paper, we outline the implementation of Hibler’s visco-plastic (VP) sea ice model into OpenFOAM, an opensource finite-volume modelling toolkit. Hibler’s visco-plastic model is arguably the most widely used description of sea ice rheology, and finds application in most global climate models. The VP model has been shown to accurately capture the bulk behaviour of sea ice at large length scales. Under convergent conditions, the VP model allows the sea ice to deform plastically, while for small strains, near drift like conditions can be captured. Unfortunately however, due to the potential for large viscosities, the VP model tends to become numerically unstable. The general consensus in literature is that an implicit solution scheme is required, which tend to become expensive when used in global climate models. Suggestions to improve the convergence behaviour include techniques such as successive over-relaxation or via the addition of an elastic term, known as the elastic-visco-plastic (EVP) method. In this paper, we aim introduce the concept of dynamic relaxation, which in addition to matrix conditioning, can be used to both stabilise and accelerate the iterative convergence behaviour. The behaviour of the sea ice model will be demonstrated on a number of test cases. DA - 2018-09 DB - ResearchSpace DP - CSIR KW - Sea ice modelling KW - OpenFOAM KW - Visco-plastic rheology KW - Dynamic relaxation LK - https://researchspace.csir.co.za PY - 2018 T1 - Implementation of a visco-plastic sea ice model into OpenFOAM TI - Implementation of a visco-plastic sea ice model into OpenFOAM UR - http://hdl.handle.net/10204/10490 ER - en_ZA


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