scholarly journals Effect of a Coccolithophore Bloom on the Underwater Light Field and the Albedo of the Water Column

2020 ◽  
Vol 8 (6) ◽  
pp. 456 ◽  
Author(s):  
Oleg Kopelevich ◽  
Sergey Sheberstov ◽  
Svetlana Vazyulya

The goal of this work is to study the influence of coccolithophore blooms on the underwater light field and albedo of the water column. A coccolithophore is a single-celled alga with spherical cells surrounded by disk-shaped calcite plates (coccolites), which produce strong light scattering. Because of that, we can observe coccolithophore blooms on satellite ocean color images. We calculated the angular underwater radiance distributions and their integral parameters by the exact numerical method with the input parameters, corresponding to real conditions observed in the Barents Sea and Black Sea. Using the results of the exact calculations, we estimated, for various situations, the accuracy of the approximating formulas applied to the assessment of the water radiance reflectance and the diffuse attenuation coefficients and we make recommendations for their application. As a finding of practical importance, we can note the estimate of the accuracy of the widely used Gordon’s formula for the diffuse attenuation coefficient; this formula results in large errors under strong coccolithophore blooms. We also mention the interesting and important results concerning the features of the asymptotic regime under such conditions.

2020 ◽  
Vol 103 (sp1) ◽  
pp. 453
Author(s):  
Ping Yang ◽  
Zizhao Wu ◽  
Yao Chen ◽  
Yilu Guo ◽  
Peng Zhang ◽  
...  

1985 ◽  
Vol 11 (2) ◽  
pp. 78-81 ◽  
Author(s):  
R. D. Robarts ◽  
T. Zohary ◽  
F. Ojeda ◽  
C. C.E. Lovengreen ◽  
R. D. Walmsley

1981 ◽  
Vol 32 (4) ◽  
pp. 517 ◽  
Author(s):  
JTO Kirk

A Monte Carlo calculation procedure has been developed for computer modelling of the penetration of light into turbid, coloured waters of the type commonly found on the Australian continent. For monochromatic light the structure of the underwater light field is described in terms of the variation of the average cosine (total, downward, upward) and irradiance reflectance, as a function of optical depth at a given ratio of scattering to absorption (bla), and as a function of bia at a given optical depth. The vertical attenuation coefficient for downward irradiance at the mid-point of the euphotic zone [Kd(za)] has been studied as a function of the absorption (a) and scattering (b) coefficients and, with the particular normalized volume scattering function used in these simulations. has been found to conform closely to the equation Kd(zm) = (a2 + 0.256ab)½ The data generated by the model have been used in conjunction with radiative transfer theory to determine the contribution of the different components of the attenuation mechanism to the vertical diminution of irradiance at different ratios of b to a. Simulation of the penetration of photosynthetically available radiation into four water bodies in the southern tablelands of New South Wales has been carried out using measured absorption coefficients and indirectly estimated values for scattering coefficients. The calculated values for vertical attenuation coefficients are in good agreement with those obtained by measurement within the water bodies. The possible use of this modelling procedure as a predictive tool is discussed.


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