1999
DOI: 10.1023/a:1018605517923
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Cited by 34 publications
(12 citation statements)
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References 27 publications
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“…The first implementation of this EB rheology into short (3 days), noadvection, stand-alone pan-Arctic simulations forced by realistic wind forcing from reanalyses was performed with an infinitely slow driving condition (external driving is artificially frozen as long as a damage cascading process proceeds). In agreement with observations, deformation was observed to strongly localize along linear-like features, to be characterized by power-law PDFs, and to follow a scaling relation ε ∼ L −β (1) . Although ice is considered as being elastically isotropic at the grid scale, stress and strain anisotropy spontaneously emerge at larger scales.…”
Section: Modelling the Scale-invariant Brittle Mechanics Of Sea Ice Wsupporting
confidence: 88%
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“…The first implementation of this EB rheology into short (3 days), noadvection, stand-alone pan-Arctic simulations forced by realistic wind forcing from reanalyses was performed with an infinitely slow driving condition (external driving is artificially frozen as long as a damage cascading process proceeds). In agreement with observations, deformation was observed to strongly localize along linear-like features, to be characterized by power-law PDFs, and to follow a scaling relation ε ∼ L −β (1) . Although ice is considered as being elastically isotropic at the grid scale, stress and strain anisotropy spontaneously emerge at larger scales.…”
Section: Modelling the Scale-invariant Brittle Mechanics Of Sea Ice Wsupporting
confidence: 88%
“…As α (1) can be considered as a measure of intermittency, varying between 0 (non-intermittent 'flow') and 1 (extreme intermittency), relation (3.3b) expresses a more continuous sea ice mechanics with increasing spatial scale. Similarly, the measure of spatial localization, β (1), is bounded between 0 (a perfectly homogeneous field) and 2 (a point-like process), and equation (3.3a) reflects a progressive smoothing as one cumulates deformation events decreasingly correlated with increasing time. The unique expression compatible with (3.3a,b) is the following coupled equation [50]:…”
Section: (A) Sea Ice Deformationmentioning
confidence: 99%
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“…Considering that the upper limit should be used in practical applications, a dynamic failure strain criterion related to the rate-independent and cumulative plastic strain is used in this paper to define the failure of the element. The criterion originates from Jordaan's empirical formula [29] and is used by Liu [19] and Gao [20], as shown in formula (10, 11) 2 , and p cut is the truncated stress. In addition, taking the tensile strength into consideration, the tensile strength limit is 2 MPa.…”
Section: Ice Materials Model Considering the Temperature Effectsmentioning
confidence: 99%
“…Sand (2008) employed plastic models to represent brittle cracking and the subsequent crushing by significantly lowering the strength parameters of the failing elements at the point of failure. Jordaan et al (1999) and Taylor and Jordaan (2014) utilised a two-term damage mechanics model, which represents both brittle and ductile behaviour simultaneously and aims to capture the phenomena occurring during high-speed compressive failure of ice. Low and high confinement processes were treated separately with separate damage variables.…”
Section: Damage Mechanics Modelsmentioning
confidence: 99%