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Real data experimentation with higher order finite differencing in the semi-implicit version of the Shuman-Hovermale Model
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1977
[PDF-2.93 MB]
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Description:"In grid point numerical models of the atmosphere, truncation errors in space result from using finite-difference approximations to the appropriate set of continuous equations. These errors usually appear as a retardation of forecasted phase speeds of meteorological features. There are several techniques available to reduce this truncation error"--Introduction.
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Content Notes:K.A. Campana.
"November 1977."
"This is an unreviewed manuscript, primarily intended for informal exchange of information among NMC staff members."
System requirements: Adobe Acrobat Reader.
Includes bibliographical references (page 9).
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Rights Information:Public Domain
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Compliance:Library
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