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2013
We consider in the present chapter, the fully three-dimensional case defined by (2.62)–(2.68). We shall consider here, for simplicity, a unique connected domain of genus 1 (i.e. a torus-like domain, see Fig. 1.1). This one is denoted by Ω.
Rachid Touzani, Jacques Rappaz
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We consider in the present chapter, the fully three-dimensional case defined by (2.62)–(2.68). We shall consider here, for simplicity, a unique connected domain of genus 1 (i.e. a torus-like domain, see Fig. 1.1). This one is denoted by Ω.
Rachid Touzani, Jacques Rappaz
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1986
After the first numerical experiment on the general circulation of the atmosphere by Phillips (1956), numerical models of the atmosphere rapidly achieved great popularity. At present numerous research and operational meteorological centers in many countries have at their disposal such models of their own construction.
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After the first numerical experiment on the general circulation of the atmosphere by Phillips (1956), numerical models of the atmosphere rapidly achieved great popularity. At present numerous research and operational meteorological centers in many countries have at their disposal such models of their own construction.
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Three-Dimensional Wheat Modelling Based on Leaf Morphological Features and Mesh Deformation
Agronomy, 2022Weiliang Wen +2 more
exaly
Modelling Electroluminescence Emission in Polymeric Material Using Dimensional Analysis Method
Energies, 2023Mohd Khairil Rahmat +2 more
exaly
1975
The classical three-dimensional theory of elasticity is generally thought of as the only one available to describe the three-dimensional behaviour of elastic bodies.
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The classical three-dimensional theory of elasticity is generally thought of as the only one available to describe the three-dimensional behaviour of elastic bodies.
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Three-Dimensional Numerical Modelling of Real-Field Dam-Break Flows: Review and Recent Advances
Water (Switzerland), 2023Massimo Tomirotti, Andrea Maranzoni
exaly