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Stable Centered-Difference Schemes, Based on an Unstaggered A Grid, That Eliminate Two-Grid Interval Noise
Publisher: American Meteorological Society
Abstract: The use of a centered-difference scheme on an unstaggered horizontal grid in time-dependent atmospheric or oceanic models leads to spurious two-grid-interval wave solutions that may appear as small-scale noise and mask the ...
A Semi-Implicit Runge–Kutta Time-Difference Scheme for the Two-Dimensional Shallow-Water Equations
Publisher: American Meteorological Society
Abstract: A semi-implicit, two time-level, three-step iterative time-difference scheme is proposed for the two-dimensional nonlinear shallow-water equations in a conservative flux form. After a semi-implicit linearization of the ...
An Explicit Time-Difference Scheme with an Adams–Bashforth Predictor and a Trapezoidal Corrector
Publisher: American Meteorological Society
Abstract: A new predictor-corrector time-difference scheme that employs a second-order Adams?Bashforth scheme for the predictor and a trapezoidal scheme for the corrector is introduced. The von Neumann stability properties of the ...
Implicit–Explicit Runge–Kutta Methods for Fast–Slow Wave Problems
Publisher: American Meteorological Society
Abstract: inear multistage (Runge?Kutta) implicit?explicit (IMEX) time integration schemes for the time integration of fast-wave?slow-wave problems for which the fast wave has low amplitude and need not be accurately simulated are ...
A Nonreflecting Upper Boundary Condition for Anelastic Nonhydrostatic Mesoscale Gravity-Wave Models
Publisher: American Meteorological Society
Abstract: A sponge layer is formulated to prevent spurious reflection of vertically propagating quasi-stationary gravity waves at the upper boundary of a two-dimensional numerical anelastic nonhydrostatic model. The sponge layer ...
A Locally One-Dimensional Semi-Implicit Scheme for Global Gridpoint Shallow-Water Models
Publisher: American Meteorological Society
Abstract: A splitting method is presented for eliminating the need to directly solve for a two-dimensional Helmholtz-type difference equation in a semi-implicit scheme for a global gridpoint shallow-water model. In the proposed ...