. Effects of weather upon the thermal structure of the ocean. Progress report no. 1. Ocean-atmosphere interaction; Ocean temperature. Here kk'q £ 14 ui » .6 i t- 2s is o 20 22 24 26 28 30. FIGURE 8. CHANGE IN TEMPERATURE DISTRIBUTION DUE TO HEAT EXCHANGE WITH ATMOSPHERE AND DUE TO CONVECTION. 20-27 APRIL 1951 (1l) Turbulent mixing (see Sec. 5 above) The character of Tc(z) was so unusual that it was considered probable from past experience that the wind and sea would be of enough force to mix the shallow layer in which two abrupt discontinuities are shown. Some of this abruptness undoubtedly is
. Effects of weather upon the thermal structure of the ocean. Progress report no. 1. Ocean-atmosphere interaction; Ocean temperature. Here kk'q £ 14 ui » .6 i t- 2s is o 20 22 24 26 28 30. FIGURE 8. CHANGE IN TEMPERATURE DISTRIBUTION DUE TO HEAT EXCHANGE WITH ATMOSPHERE AND DUE TO CONVECTION. 20-27 APRIL 1951 (1l) Turbulent mixing (see Sec. 5 above) The character of Tc(z) was so unusual that it was considered probable from past experience that the wind and sea would be of enough force to mix the shallow layer in which two abrupt discontinuities are shown. Some of this abruptness undoubtedly is due to the discontinuous manner in which the temperature changes due to radiation must be plotted. Therefore, T (z) was adjusted by graphic means according to the 30. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original United States. Hydrographic Office; Schule, John J; Simpson, Lloyd S; Shapiro, A; United States. Hydrographic Office. Washington, D. C. , U. S. Navy Hydrographic Office
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