. Effects of weather upon the thermal structure of the ocean. Progress report no. 1. Ocean-atmosphere interaction; Ocean temperature. 'UoFACE LIGHT5%) ,o jp. 100 data- for the red, yellow, green, and blue portions of the spectra. For each of these bands the graph shows the percentage, on a log- arithmic scale, of the in- coming radiation that is figure 5. transparency station. 23 april i95i. left at any depth. The problem is to determine how much of the radiation is concentrated in each band. Figure 6 is an adaptation of a graph presented on page 105 of The Oceans (191+2) showing the distr
. Effects of weather upon the thermal structure of the ocean. Progress report no. 1. Ocean-atmosphere interaction; Ocean temperature. 'UoFACE LIGHT5%) ,o jp. 100 data- for the red, yellow, green, and blue portions of the spectra. For each of these bands the graph shows the percentage, on a log- arithmic scale, of the in- coming radiation that is figure 5. transparency station. 23 april i95i. left at any depth. The problem is to determine how much of the radiation is concentrated in each band. Figure 6 is an adaptation of a graph presented on page 105 of The Oceans (191+2) showing the distribution of the energy spectrum at the surface of the radiation from sun and sky, plotted a*- a function of wave length. Taking + micron as the lower end of the red band and measuring the area under the curve, one arrives at a fig- ure of 61+03$ for the red and $ for. 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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