Panoramic diagnostics of surface temperatures and heat fluxes in an aerodynamic experiment
β Scribed by G. M. Zharkova; V. N. Kovrizhina
- Book ID
- 106411198
- Publisher
- Springer US
- Year
- 2010
- Tongue
- English
- Weight
- 639 KB
- Volume
- 83
- Category
- Article
- ISSN
- 1573-871X
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π SIMILAR VOLUMES
## OkE Non-dimensional absolute humidity gradient. OH Non-dimensional temperature gradient of heat flux. ObM Non-dimensional wind shear. ~b ~' = OM = H = WE, an assumption used in stable conditions. Q Air density. e, Absolute humidity. Qw Density of water. T Kinematic shear stress. Logarithmic hei
The 'force-restore' approach is commonly used in order to calculate the surface temperature in atmospheric models. A critical point in this method is how to calculate the deep soil temperature which appears in the restore term of the 'force-restore' equation. If the prognostic equation for calculati