A finite-difference GCM dynamical core with a variable-resolution stretched grid
In other words, the longer-term integrations suffer from an inaccurate interaction at the boundaries of the area of interest. [...]a nested-grid approach does not allow one to perform continuous long-term integrations without updating initial and boundary conditions. [...]the fine-resolution fields...
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Veröffentlicht in: | Monthly weather review 1997-11, Vol.125 (11), p.2943-2968 |
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container_title | Monthly weather review |
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creator | FOX-RABINOVITZ, M. S STENCHIKOV, G. L SUAREZ, M. J TAKACS, L. L |
description | In other words, the longer-term integrations suffer from an inaccurate interaction at the boundaries of the area of interest. [...]a nested-grid approach does not allow one to perform continuous long-term integrations without updating initial and boundary conditions. [...]the fine-resolution fields may provide only a marginal to moderate impact on the coarse-resolution fields within a buffer zone around the area of interest. |
doi_str_mv | 10.1175/1520-0493(1997)125<2943:AFDGDC>2.0.CO;2 |
format | Article |
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source | American Meteorological Society; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
subjects | Advantages Atmospheric models Boundary conditions Coordinate transformations Earth, ocean, space Exact sciences and technology External geophysics Fluid dynamics Geophysics. Techniques, methods, instrumentation and models Meteorology |
title | A finite-difference GCM dynamical core with a variable-resolution stretched grid |
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