Vs. Kuwahara et al., Variability of bio-optical factors influencing the seasonal attenuation ofultraviolet radiation in temperate coastal waters of Japan, PHOTOCHEM P, 72(2), 2000, pp. 193-199
The study identifies the relative contribution of various bio-optical facto
rs to the total attenuation of ultraviolet radiation (UVR) wavelengths and
photosynthetically active radiation (PAR) in temperate coastal waters of Ja
pan by surveying the physical properties of the water column, UVR and PAR p
enetration, 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 sea
sonal and wavelength specific variability, On an annual basis, absorbance b
y a(CDOM) I was the highest absorbing fraction (47-59%) for the UVR wavelen
gths measured (305, 320, 340 and 380 nm) hut decreased (32%) at 450 nm, Con
tribution of pigments to total absorbance was highest (40-60%) during a spr
ing bloom for both UVR and PAR. A large variability (C.V. > 42%) for annual
average attenuation coefficients (K-d[lambda]) at respective wavelengths o
bserved suggests that the spectral composition of the water column changes
throughout the year in this region, A significant relationship was observed
between K-d(lambda) 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 variat
ions in K-d(lambda), particularly in the UVR range, The slope S, obtained f
rom a natural-log plot of the absorption coefficient of CDOM against wavele
ngth, ranged between 0.014 and 0.036 nm(-1) annually (average = 0.020+/-0.0
07, C.V. = 35%) and suggests seasonal changes in the origin of CDOM between
terrestrial (low S) and biogenous thigh S) CDOM.