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Variability of Bio‐optical Factors Influencing the Seasonal Attenuation of Ultraviolet Radiation in Temperate Coastal Waters of Japan ¶
Author(s) -
Kuwahara Victor S.,
Ogawa Hiroshi,
Toda Tatsuki,
Kikuchi Tomohiko,
Taguchi Satoru
Publication year - 2000
Publication title -
photochemistry and photobiology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.818
H-Index - 131
eISSN - 1751-1097
pISSN - 0031-8655
DOI - 10.1562/0031-8655(2000)0720193vobofi2.0.co2
Subject(s) - colored dissolved organic matter , photosynthetically active radiation , absorbance , water column , attenuation , environmental science , attenuation coefficient , temperate climate , wavelength , absorption (acoustics) , ultraviolet radiation , ultraviolet , seasonality , atmospheric sciences , dissolved organic carbon , environmental chemistry , oceanography , chemistry , phytoplankton , ecology , biology , photosynthesis , optics , geology , nutrient , physics , chromatography , biochemistry , organic chemistry , radiochemistry
The study identifies the relative contribution of various bio‐optical factors to the total attenuation of ultraviolet radiation (UVR) wavelengths and photosynthetically active radiation (PAR) in temperate coastal waters of Japan by surveying the physical properties of the water column, UVR and PAR penetration, and the absorption characteristics of dissolved and particulate material. Spectral absorbance properties of pigment ( a ph ), detritus ( a d ) and chromophoric dissolved organic material ( a CDOM ) displayed both seasonal and wavelength specific variability. On an annual basis, absorbance by a CDOM was the highest absorbing fraction (47–59%) for the UVR wavelengths measured (305, 320, 340 and 380 nm) but decreased (32%) at 450 nm. Contribution of pigments to total absorbance was highest (40–60%) during a spring bloom for both UVR and PAR. A large variability (C.V. > 42%) for annual average attenuation coefficients ( K d [λ]) at respective wavelengths observed suggests that the spectral composition of the water column changes throughout the year in this region. A significant relationship was observed between K d (λ) and a CDOM at 305, 320, 340 and 380 nm only ( P < 0.01) but not for 450 nm (PAR) indicating the role of CDOM in regulating variations in K d (λ), particularly in the UVR range. The slope S, obtained from a natural‐log plot of the absorption coefficient of CDOM against wavelength, ranged between 0.014 and 0.036 nm −1 annually (average = 0.020±0.007, C.V. = 35%) and suggests seasonal changes in the origin of CDOM between terrestrial (low S ) and biogenous (high S ) CDOM.