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contributor authorLander, J.
contributor authorHoskins, B. J.
date accessioned2017-06-09T16:11:11Z
date available2017-06-09T16:11:11Z
date copyright1997/02/01
date issued1997
identifier issn0027-0644
identifier otherams-62850.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4203787
description abstractThrough analysis of the spectra of a Dirac delta function the notion of believable and unbelievable scales in a spectral transform model is quantified. The smallest resolved local features are shown to have an average wavenumber a factor of 2 less than that of the truncation, and a half-width 1.6 times greater than that associated with the smallest-scale waves and 2.4 times the maximum grid size of a quadratic transform grid. A reassessment of the philosophy of including parameterizations is introduced, the central point of which is a separation of the parameterization and dynamical truncation scales. The use of spectral filters applied to the input and output from gridpoint physical parameterization schemes and the use of a coarse ?physics? grid are proposed. Diagnostics summarizing the noise in a spectral model are introduced, and a moist baroclinic wave life-cycle simulation and a one-dimensional analog to photochemistry at the terminator are discussed to demonstrate their use.
publisherAmerican Meteorological Society
titleBelievable Scales and Parameterizations in a Spectral Transform Model
typeJournal Paper
journal volume125
journal issue2
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(1997)125<0292:BSAPIA>2.0.CO;2
journal fristpage292
journal lastpage303
treeMonthly Weather Review:;1997:;volume( 125 ):;issue: 002
contenttypeFulltext


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