Stability Conditions for an Alternated Grid in Space and Time

The stability conditions of a staggered lattice in space and time are derived. The grid used is known as the Eliassen grid (Eliassen 1956). It is shown that the stability conditions of the shallow water wave equations, for this type of lattice, have essentially the same stability condition as the...

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Main Authors: Camerlengo, Alejandro Livio, Ines Demmler, Monica
Format: Article
Language:English
English
Published: Universiti Putra Malaysia Press 1995
Online Access:http://psasir.upm.edu.my/id/eprint/3858/
http://psasir.upm.edu.my/id/eprint/3858/1/Stability_Conditions_for_an_Alternated.pdf
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author Camerlengo, Alejandro Livio
Ines Demmler, Monica
author_facet Camerlengo, Alejandro Livio
Ines Demmler, Monica
author_sort Camerlengo, Alejandro Livio
building UPM Institutional Repository
collection Online Access
description The stability conditions of a staggered lattice in space and time are derived. The grid used is known as the Eliassen grid (Eliassen 1956). It is shown that the stability conditions of the shallow water wave equations, for this type of lattice, have essentially the same stability condition as the unstaggered grid and Arakawa's B and C lattice. Upon implementation of a leapfrog scheme in a staggered grid in space and time, there will be no computational modes. No smoothing is needed to compute the Coriolis (gravity wave) terms as required in Arakawa's C (B) grid. Furthermore, the usage of an Eliassen grid halves the computation time required in Arawaka's B or C grid (Mesinger and Arakawa 1976). Therefore, there are fundamental advantages for the usage of an alternated grid in space and time.
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English
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spelling upm-38582013-05-27T07:11:48Z http://psasir.upm.edu.my/id/eprint/3858/ Stability Conditions for an Alternated Grid in Space and Time Camerlengo, Alejandro Livio Ines Demmler, Monica The stability conditions of a staggered lattice in space and time are derived. The grid used is known as the Eliassen grid (Eliassen 1956). It is shown that the stability conditions of the shallow water wave equations, for this type of lattice, have essentially the same stability condition as the unstaggered grid and Arakawa's B and C lattice. Upon implementation of a leapfrog scheme in a staggered grid in space and time, there will be no computational modes. No smoothing is needed to compute the Coriolis (gravity wave) terms as required in Arakawa's C (B) grid. Furthermore, the usage of an Eliassen grid halves the computation time required in Arawaka's B or C grid (Mesinger and Arakawa 1976). Therefore, there are fundamental advantages for the usage of an alternated grid in space and time. Universiti Putra Malaysia Press 1995 Article PeerReviewed application/pdf en http://psasir.upm.edu.my/id/eprint/3858/1/Stability_Conditions_for_an_Alternated.pdf Camerlengo, Alejandro Livio and Ines Demmler, Monica (1995) Stability Conditions for an Alternated Grid in Space and Time. Pertanika Journal of Science & Technology, 3 (2). pp. 271-283. ISSN 0128-7680 English
spellingShingle Camerlengo, Alejandro Livio
Ines Demmler, Monica
Stability Conditions for an Alternated Grid in Space and Time
title Stability Conditions for an Alternated Grid in Space and Time
title_full Stability Conditions for an Alternated Grid in Space and Time
title_fullStr Stability Conditions for an Alternated Grid in Space and Time
title_full_unstemmed Stability Conditions for an Alternated Grid in Space and Time
title_short Stability Conditions for an Alternated Grid in Space and Time
title_sort stability conditions for an alternated grid in space and time
url http://psasir.upm.edu.my/id/eprint/3858/
http://psasir.upm.edu.my/id/eprint/3858/1/Stability_Conditions_for_an_Alternated.pdf