Abstract
The cooling capacity of an atmospheric environment is examined with respect to a wet object of a given surface temperature. The maximum cooling capacity (MCC) is defined as the sum of the sensible and latent heat fluxes out of a unit area of the object. It is found that, for a given surface temperature and wind speed, the MCC is essentially a function of the wet bulb temperature of the ambient air with a very weak dependence on the ambient air temperature and pressure.-from Author
Original language | English |
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Pages (from-to) | 1387-1391 |
Number of pages | 5 |
Journal | Journal of Applied Meteorology |
Volume | 23 |
Issue number | 9 |
DOIs | |
State | Published - 1 Jan 1984 |
ASJC Scopus subject areas
- General Engineering