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dc.contributor.authorNelson, Stephan P.
dc.contributor.authorWeible, Michael L.
dc.date.accessioned2017-06-09T17:40:28Z
dc.date.available2017-06-09T17:40:28Z
dc.date.copyright1980/04/01
dc.date.issued1979
dc.identifier.issn0021-8952
dc.identifier.otherams-9893.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4233431
dc.description.abstractEquations for the three-dimensional Shuman filter and its response function are presented. The filter heavily dampens even fairly long waves, but this can be alleviated somewhat by a second amplifying pass (tandem filter). Due to the number of points (27) needed to filter the data, irregular boundaries and missing data can be a problem. The effects of one possible solution (reverting to three one-dimensional filters) is shown. Under some instances it is preferable to make only one pass to prevent propagation of boundary discontinuities.
dc.publisherAmerican Meteorological Society
dc.titleThree-Dimensional Shuman Filter
dc.typeJournal Paper
dc.journal.volume19
dc.journal.issue4
dc.journal.titleJournal of Applied Meteorology
dc.identifier.doi10.1175/1520-0450(1980)019<0464:TDSF>2.0.CO;2
dc.journal.fristpage464
dc.journal.lastpage469
dc.treeJournal of Applied Meteorology:;1979:;volume( 019 ):;issue: 004
dc.contenttypeFulltext


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