1976년 9월 20일 부터 24일 사이에 북서태평양(Kamchatka 근해에서 투명도, 태양광선의 적색광(과장 : 600\~620\;nm)에 대한 표면조도 및 수심별 수중조도와 태양고도, 기온 및 표층수온 등을 조사한 결과를 요약하면 다음과 같다. 1. 본 조사해역의 평균투명도는 $10.6m(9\~l2m)\$로 나타났다. 2. 태양광선의 적색광에 대한 해수의 흡수계수는 $0.178\~0.376$(평균 0.278)였다. 3. 적색광에 대한 해수의 흡수계수 m와 투명도 D와의 관계는 m=3.347/D로 나타났다. 4. 관측된 평균기온은 $9.49^{\circ}C(7.8-12.6^{\circ}C)$ 였고, 평균표층수온은 $6.58^{\circ}(5.8-7.6^{\circ}C$)로 나타났다. 5. m층에서 적색광에 대한 수중투과율은 수심 5 m층에서 표면창의 $6.45\~23.5\%$(평균 $16.36\%$), 수심 10 m층에서는 $1.38\~7.31포$(평균 $3.65\%$)였고, 수심 20 m층에서는 $0.048\~0.647\% $(평균 0.276\%)로 나타났다.
1976년 9월 20일 부터 24일 사이에 북서태평양(Kamchatka 근해에서 투명도, 태양광선의 적색광(과장 : 600\~620\;nm)에 대한 표면조도 및 수심별 수중조도와 태양고도, 기온 및 표층수온 등을 조사한 결과를 요약하면 다음과 같다. 1. 본 조사해역의 평균투명도는 $10.6m(9\~l2m)\$로 나타났다. 2. 태양광선의 적색광에 대한 해수의 흡수계수는 $0.178\~0.376$(평균 0.278)였다. 3. 적색광에 대한 해수의 흡수계수 m와 투명도 D와의 관계는 m=3.347/D로 나타났다. 4. 관측된 평균기온은 $9.49^{\circ}C(7.8-12.6^{\circ}C)$ 였고, 평균표층수온은 $6.58^{\circ}(5.8-7.6^{\circ}C$)로 나타났다. 5. m층에서 적색광에 대한 수중투과율은 수심 5 m층에서 표면창의 $6.45\~23.5\%$(평균 $16.36\%$), 수심 10 m층에서는 $1.38\~7.31포$(평균 $3.65\%$)였고, 수심 20 m층에서는 $0.048\~0.647\% $(평균 0.276\%)로 나타났다.
Optical properties were studied in the Northwest Pacific near Kamchatka Peninsula based on ten oceanographic stations from September 20 to 24, 1976. Submarine light intensity was measured by usins a submarine illuminometer (RIGO, Type: 2501-A) ; equipped with a red filter (RIGO, Type: V-R-60, wave l...
Optical properties were studied in the Northwest Pacific near Kamchatka Peninsula based on ten oceanographic stations from September 20 to 24, 1976. Submarine light intensity was measured by usins a submarine illuminometer (RIGO, Type: 2501-A) ; equipped with a red filter (RIGO, Type: V-R-60, wave length: 600-620 nm). Light intensity in the upper 40 m depth layer was measured at 1 m depth intervals. The absorption coefficient for red color in the area ranged from 0. 178 to 0.376 (mean 0.278) : the Secchidisc depth in the area ranged from 9 to 12 meters (mean 10.6 meters). The relationship between absorption coefficient (m) and transparency depth (D) was m=5.347/D. The rates of light penetration for red color at three different depths are computed with reference to the surface light intensity. The mean rates of light penetration were $16.36\%\;(6.45\~23.5\%),\;3.65\%\;(1.38\~7.31\%)\;and\;0.276\%(0.048\~0.647\%) $ at the depths of s m, 10 m, and 20 m, respectively.
Optical properties were studied in the Northwest Pacific near Kamchatka Peninsula based on ten oceanographic stations from September 20 to 24, 1976. Submarine light intensity was measured by usins a submarine illuminometer (RIGO, Type: 2501-A) ; equipped with a red filter (RIGO, Type: V-R-60, wave length: 600-620 nm). Light intensity in the upper 40 m depth layer was measured at 1 m depth intervals. The absorption coefficient for red color in the area ranged from 0. 178 to 0.376 (mean 0.278) : the Secchidisc depth in the area ranged from 9 to 12 meters (mean 10.6 meters). The relationship between absorption coefficient (m) and transparency depth (D) was m=5.347/D. The rates of light penetration for red color at three different depths are computed with reference to the surface light intensity. The mean rates of light penetration were $16.36\%\;(6.45\~23.5\%),\;3.65\%\;(1.38\~7.31\%)\;and\;0.276\%(0.048\~0.647\%) $ at the depths of s m, 10 m, and 20 m, respectively.
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