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2017
DOI: 10.1088/1742-6596/929/1/012103
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Analytical and numerical solutions to Stefan problem in model of the glaciation dynamics of the multilayer cylinder in sea water

Abstract: Abstract. A mathematical model of the glaciation dynamics of the multilayer cylinder is suggested. The model reflects the specific feature of glaciation in salt water. The choice of effective model parameters and thermal characteristics of the increasing ice is considered. The calculations of problem using front-tracking finite difference method and using analytical solution found in quasi-stationary approximation are presented.

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Cited by 7 publications
(4 citation statements)
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“…In this sense, the considered model is close to the model of a phase transition with a moving boundary [36][37][38][39], the position of which is determined by the field profile. The position of the phase transition boundary is not determined in advance, but it is determined in the course of solution of such problems.…”
Section: Introductionmentioning
confidence: 85%
“…In this sense, the considered model is close to the model of a phase transition with a moving boundary [36][37][38][39], the position of which is determined by the field profile. The position of the phase transition boundary is not determined in advance, but it is determined in the course of solution of such problems.…”
Section: Introductionmentioning
confidence: 85%
“…It is known that all thermal and physical characteristics of growing sea ice depend on its salinity. The authors have previously proposed [15] the selection technique of a consistent set of thermo physical characteristics of growing sea ice. Based on these data, the following set of thermo physical characteristics and conditions was used in the calculations:…”
Section: Problem Statementmentioning
confidence: 99%
“…We estimate the error with which the Stefan condition (8) is satisfied in the numerical solution to the smoothed eq. (15). We write the integral equation of the balance of internal energy, ε , of the resting medium in the absence of sources (sinks) and external forces.…”
Section: Analysis Of the Cause Of The Increasing Error In The Calculamentioning
confidence: 99%
“…Для определения начальных распределений температур T i 0 и максимальной толщины слоя льда сначала решается задача оледенения (постановка и алгоритм решения задачи приведены в работе [1]). Если температура окружающей воды увеличивается настолько, что для соответствующего ей значения величины теплового потока q 3 выполняется неравенство:…”
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