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Instability of water cooled from above

Conference ·
OSTI ID:4084863
The temperature field and convection currents induced in water by convection, evaporation and radiation cooling of its surface were studied. These phenomena occur naturally and continuously in any lake, pond, reservoir or a river but they remain usually unobserved. Mach--Zehnder interferograms taken from the side of a tank of water are here used to measure the temperature distribution and to study the convective currents induced by cooling from the surface. Experiments were performed with initially uniform and thermally- stratified layers of water. Both qualitative and quantitative results of preliminary nature for temperature distribution are presented. Interferograms vividly reveal mixing motions induced by instabilities arising in the surface layer. The onset of manifest convective behavior was determined by visual observations of interferograms. (auth)
Research Organization:
Purdue Univ., West Lafayette, IN
NSA Number:
NSA-33-020207
OSTI ID:
4084863
Report Number(s):
CONF-7309143--P4
Country of Publication:
United States
Language:
English