Adaptive Atmospheric Modeling: Key Techniques in Grid by Jörn Behrens PDF

By Jörn Behrens

ISBN-10: 3540333827

ISBN-13: 9783540333821

ISBN-10: 3540333835

ISBN-13: 9783540333838

This booklet offers an outline and distinctive counsel towards the advance of adaptive innovations for atmospheric modeling. Written in an academic kind and that includes an exhaustive checklist of references, it capabilities as a kick off point for everybody who's drawn to adaptive modeling, in atmospheric sciences and past.

The insurance comprises paradigms of adaptive suggestions, reminiscent of mistakes estimation and version standards. Mesh new release tools are offered for triangular/tetrahedral and quadrilateral/hexahedral meshes, with a different part on preliminary meshes for the field. The ebook discusses potency matters, together with options for accelerating unstructured mesh computations in addition to parallelization. Written in an applications-focused demeanour, the ebook demonstrates numerous concepts for discretizing appropriate conservation legislation from atmospheric modeling.

Finite quantity, discontinuous Galerkin and conservative Semi-Lagrangian equipment are brought and utilized in simplified actual lifestyles simulations. The ebook is designed to inspire the reader to get involved with adaptive modeling techniques.

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Additional info for Adaptive Atmospheric Modeling: Key Techniques in Grid Generation, Data Structures, and Numerical Operations with Applications

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11. 16 For uneven numbers of sub-cells in each patch cell, a convenient closure method can be derived that avoids triangular closures. 15 that can easily be generalized to higher uneven numbers. It should be mentioned, however, that for high numbers ν = 2k + 1, k ∈ N very thin quadrilaterals can occur which might degrade numerical stability. See fig. 11 for an example with a 5 × 5-patch. Finally, in order to obtain an algorithm that creates an admissible mesh, the refinement and closure strategies have to be combined.

This method is especially suited for mesh-free methods, where only point locations are considered for calculations. 24 (Admissible unstructured triangulation) Let T = {τ1 , . . , τM } be a given admissible coarse triangulation, and let S ⊂ T be the set of cells marked for refinement. Fig. 14. Local refinement of a Delaunay triangulation by insertion of centroid and re-meshing 38 3 Grid Generation v4 v4 v3 v1 v2 v4 Fig. 15. Unfolding a tetrahedron into standard position, and notations for local vertex ordering and globally marked edge (dotted line) 1.

4. Jablonowski assesses three different physical adaptation criteria, the (relative) vorticity ζr , the gradient of the geopotential height field ∇Φ and the curvature of the geopotential height, in other words the Laplacian ∆Φ [221]. Her auter. conclusions result in an error criterion based on either ∇Φ or ζr , as in L¨ However, she reports on alternating refinement/de-refinement behavior in her simulations as well as mislead refinement by high frequency oscillations in the solution due to numerical (instability) effects.

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Adaptive Atmospheric Modeling: Key Techniques in Grid Generation, Data Structures, and Numerical Operations with Applications by Jörn Behrens


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