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A note on the finite differencing of the linearized primitive equations' lower boundary conditionThis note examines the accuracy of finite difference solutions of the midlatitude primitive equations and the quasi-geostrophic equation. First order accurate forward differencing of the equations' lower boundary condition is shown to poorly simulate the radiating wave response to midlatitude heating. Forward differencing always exaggerates the magnitude of the radiating response. For a realistic heating height scale and for a reasonable mesh size this exaggeration is on the order of 50 percent. Central differencing of the lower boundary condition gives an error of only about 3 percent.
Document ID
19860044225
Acquisition Source
Legacy CDMS
Document Type
Reprint (Version printed in journal)
External Source(s)
Authors
Jacqmin, D.
(NASA Lewis Research Center Cleveland, OH; Harvard University, Cambridge, MA, United States)
Date Acquired
August 12, 2013
Publication Date
January 1, 1985
Publication Information
Publication: Pure and Applied Geophysics
Volume: 123
Issue: 3 19
ISSN: 0033-4553
Subject Category
Meteorology And Climatology
Report/Patent Number
ISSN: 0033-4553
Accession Number
86A28963
Funding Number(s)
CONTRACT_GRANT: NSF ATM-82-05638
CONTRACT_GRANT: NGL-22-007-228
Distribution Limits
Public
Copyright
Other

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