Abstract
It is demonstrated theoretically that, in the formalism of Penman-Monteith, there exists, at a free water surface, a small but finite surface resistance to both latent and sensible heat fluxes. These resistances, estimated to be of order 0.05 and 0.02 s m-1, respectively, are usually negligible but may be used to provide the hitherto unavailable theoretical description of the energy budget at a partially wet surface.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 81-99 |
| Number of pages | 19 |
| Journal | Boundary-Layer Meteorology |
| Volume | 8 |
| Issue number | 1 |
| DOIs | |
| State | Published - Jan 1975 |
| Externally published | Yes |
ASJC Scopus subject areas
- Atmospheric Science
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