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contributor authorThuburn, John
contributor authorStaniforth, Andrew
date accessioned2017-06-09T16:15:17Z
date available2017-06-09T16:15:17Z
date copyright2004/02/01
date issued2004
identifier issn0027-0644
identifier otherams-64235.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4205327
description abstractDiscretizations of the linearized shallow-water equations on a spherical C grid are considered. Constraints on the schemes' coefficients that ensure conservation of mass, angular momentum, and energy are derived. These results generalize previously published results to the case of nonuniform and rotated grids (but are restricted to the linearized equations). Grids with ? stored at the poles and grids with u and h stored at the poles are both considered. Energy conservation is shown to be problematic for grids with u and h at the poles. It is also shown that an inappropriate averaging of the Coriolis terms leads to a misrepresentation of the Rossby modes with shortest meridional scale. The appropriate averaging is shown to be compatible with the constraints required for conservation, and, indeed, the energy-conserving averaging of the Coriolis terms improves the dispersion properties of Rossby modes.
publisherAmerican Meteorological Society
titleConservation and Linear Rossby-Mode Dispersion on the Spherical C Grid
typeJournal Paper
journal volume132
journal issue2
journal titleMonthly Weather Review
identifier doi10.1175/1520-0493(2004)132<0641:CALRDO>2.0.CO;2
journal fristpage641
journal lastpage653
treeMonthly Weather Review:;2004:;volume( 132 ):;issue: 002
contenttypeFulltext


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