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
Hauptverfasser: FOX-RABINOVITZ, M. S, STENCHIKOV, G. L, SUAREZ, M. J, TAKACS, L. L
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container_end_page 2968
container_issue 11
container_start_page 2943
container_title Monthly weather review
container_volume 125
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
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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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