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- W2145654874 abstract "Measurements from the U.S.S. Rehoboth taken while anchored at about 34°N, 62°W, for twelve days in June 1953 are used to compute reflectivities of the water surface for different sun altitudes and sky conditions. These are compared with similar measurements made by Anderson over Lake Hefner and with published values of the albedo for diffuse radiation. Measurements over the ocean gave a reflectivity of about 7 per cent for diffuse radiation, which compares favorably with the reflectivity recomputed by Burt from Schmidt's work. An upper limit of about 10 per cent is suggested for sea level variations in solar radiation caused by local changes in the amount of precipitable water vapor in the atmosphere within a 24-hour period. Diurnal variations in radiant energy are reflected in comparable variations in water temperature if the radiant heat is logarithmically distributed with depth. Below the mixed layer diurnal variations in temperature are obscured by the more pronounced variations caused by motion of the water." @default.
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- W2145654874 date "1962-11-01" @default.
- W2145654874 modified "2023-09-24" @default.
- W2145654874 title "Variations in radiant energy and related ocean temperatures" @default.
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- W2145654874 doi "https://doi.org/10.1029/jz067i012p04705" @default.
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