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contributor authorSmolarkiewicz, Piotr K.
contributor authorRasch, Philip J.
date accessioned2017-06-09T14:30:15Z
date available2017-06-09T14:30:15Z
date copyright1991/03/01
date issued1991
identifier issn0022-4928
identifier otherams-20501.pdf
identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4156737
description abstractThe purpose of this paper is twofold. First, a formalism is presented that extends the conceptual framework identified by Ritchie as the ?semi-Lagrangian method without interpolation.? While his words for this concept refer to a particular class of semi-Lagrangian approximations, the idea is actually much more general. The formalism may be used to convert any advection algorithm into the semi-Lagrangian format, and it makes most algorithms sufficient for the integration of flows characterized by large Courant numbers. The formalism is presented in an arbitrary curvilinear system of coordinates. Second, exploiting the generality of the theoretical considerations, the formalism is implemented in solving a practical problem of scalar advection in spherical geometry. Rather than elaborating on Ritchie's semi-Lagrangian techniques employing centered-in-time differencing, the focus is on the alternative of forward-in-time, dissipative finite-difference schemes. This class of schemes offers attractive computational properties in terms of the solutions' accuracy and preservation of a sign or monotonicity.
publisherAmerican Meteorological Society
titleMonotone Advection on the Sphere: An Eulerian Versus Semi-Lagrangian Approach
typeJournal Paper
journal volume48
journal issue6
journal titleJournal of the Atmospheric Sciences
identifier doi10.1175/1520-0469(1991)048<0793:MAOTSA>2.0.CO;2
journal fristpage793
journal lastpage810
treeJournal of the Atmospheric Sciences:;1991:;Volume( 048 ):;issue: 006
contenttypeFulltext


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