| Автор | Lakshman, G. |
| Дата выпуска | 1971 |
| dc.description | Wind induced thermal mixing in a pond or slough influences the diurnal variation in the water surface temperature. This, in turn, greatly affects the rate of evaporation from the water surface. The maximum diurnal rise in the water temperature depends on the total duration of sunshine, the maximum rise in air temperature above the initial water temperature, and the wind speed. Sheltering a pond may increase the rate of evaporation under certain conditions. |
| Формат | application.pdf |
| Копирайт | Copyright 1971 by the American Geophysical Union. |
| Название | Some Observations on the Effect of Wind Induced Thermal Mixing |
| Тип | shortCommunication |
| DOI | 10.1029/WR007i001p00189 |
| Electronic ISSN | 1944-7973 |
| Print ISSN | 0043-1397 |
| Журнал | Water Resources Research |
| Том | 7 |
| Первая страница | 189 |
| Последняя страница | 194 |
| Выпуск | 1 |
| Библиографическая ссылка | Rosenberg, Norman J., H. E.Hart, K. W.Brown, Evapotranspiration, Review of Research, 80University of Nebraska, College of Agriculture and Home Economics, Agricultural Experiment StationNovember, 1968. |
| Библиографическая ссылка | , U.S. Geological Survey, Waterloss investigations, Lake Hefner studies, Technical report, U.S. Geol. Surv. Prof. Pap., 269, 58, 1954. |
