Abstract
Differences between surface and subsurface water-temperature are causcd by evaporation, long-wave radiation and exchange of sensible heat. The relative importance of these three components is discussed, especially with aid of observations under neutral conditions. Evaporation as well as hack radiation contributes to a cooling of the surface of 0.1 to 0.2 centigrade under neutral conditions, while under diahatic conditions greater surface temperature deviations are caused by heat exchange.
DOI: https://doi.org/10.3402/tellusa.v15i4.8859 | Journal eISSN: 3035-9554
Language: English
Page range: 363 - 366
Published on: Jan 1, 1963
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 1963 Lutz Hasse, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.