The non‐conservation of potential vorticity by a dynamical core compared with the effects of parametrized physical processes
Numerical models of the atmosphere combine a dynamical core, which approximates solutions to the adiabatic, frictionless governing equations for fluid dynamics, with tendencies arising from the parametrization of other physical processes. Since potential vorticity (PV) is conserved following fluid f...
| Main Authors: | , , |
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| Format: | Journal article |
| Published: |
Royal Meteorological Society
2016
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