## Abstract A parametrization equation for momentum flux due to convectively generated gravity waves is derived and tested numerically. the wave momentum flux just above the convective layer is shown to depend directly on the shear and the intensity of convection, and inversely on the stability of
The numerical stability of a parametrization of convective momentum transport
โ Scribed by R. Kershaw; A. L. M. Grant; S. H. Derbyshire; S. Cusack
- Book ID
- 104576478
- Publisher
- John Wiley and Sons
- Year
- 2000
- Tongue
- English
- Weight
- 241 KB
- Volume
- 126
- Category
- Article
- ISSN
- 0035-9009
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โฆ Synopsis
Abstract
The Gregory el at. parametrization of momentum transport by convection is shown to be more prone to numerical instability than other parts of the convection scheme, because of an additional element of numerical diffusion. The limiting Courant number for linear stability is (I + c)^โ1^, where c is the parameter which controls the dependence of the pressure gradient on environment shear. Some revised numerical treatments cure the instability problem but reduce forecast skill, apparently because the diffusive element of the original formulation is beneficial, even though it is artificial. A possible solution to the problem is to use an implicit treatment of the original formulation which is absolutely stable.
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