Titlebook: Continuum Mechanics and Applications in Geophysics and the Environment; Brian Straughan (Professor),Ralf Greve,Yongqi Wang Book 2001 Sprin

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https://doi.org/10.1007/978-3-322-99940-5non-stiff case, has been developed (Liotta et al., 1999a, b). Here we use such a scheme for getting numerical solutions of the shock structure problem for the model of a radiating gas described by a variable Eddington factor (Anile et al., 1991, 1992; Kremer and Müller, 1992) in the framework of extended thermodynamics.

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Numerical Investigation of Shock Waves in a Radiating Gas Described by a Variable Eddington Factornon-stiff case, has been developed (Liotta et al., 1999a, b). Here we use such a scheme for getting numerical solutions of the shock structure problem for the model of a radiating gas described by a variable Eddington factor (Anile et al., 1991, 1992; Kremer and Müller, 1992) in the framework of extended thermodynamics.

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https://doi.org/10.1007/978-3-476-00146-7amely convective motion of brine in a layer of salty sediments off the coast of Alaska (Hutter and Straughan, 1997, 1999) and inclined temperature gradient convection (Nield, 1994, 1998a). The methods are applicable to many, many more practical porous convection problems and some are mentioned.

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Melodiebildung und Orchestrationisk of collision with maritime traffic or fixed offshore structures. In the Heinrich problem the objective is to predict the temporally-evolving spatial pattern of iceberg meltwater and the associated pattern and provenance of ice-rafted marine sedimentation.