A thermodynamic diagnostic model for the atmosphere. Part III: DIAMOD with orography and new error model
The diagnostic model DIAMOD has been developed in Parts l and II of this study. Its core is the convection equation for the vertical sub-gridscale flux of moist enthalpy, called total convective heat flux h. The convection equation is forced by the analyzed gridscale total heat budget. It has been i...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Borntraeger
1995-09-01
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| Series: | Meteorologische Zeitschrift |
| Subjects: | |
| Online Access: | http://dx.doi.org/10.1127/metz/4/1995/162 |