亚速海颗粒和有色溶解有机物的光谱光吸收系数

©. T. Ya, Churilova, T. Efimova, N. Moiseeva, E. Skorokhod, A. Kovalevsky, Скороход Е.Ю Churilova, T.Ya
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引用次数: 2

摘要

基于2016 - 2020年亚速海南部不同季节浮游植物叶绿素-a (tcl -a)浓度、光吸收光谱系数、非藻颗粒(NAP)和有色溶解有机质(CDOM)的测量结果,开展了研究。获得了亚速海所有光学活性组分光吸收光谱系数变化的新数据。所有研究参数的高(超过一个数量级)可变性显示。tch -a的季节动态在冬季和夏季最大。揭示了浮游植物吸收与tcl - A之间的关系,该关系用幂函数表示。结果表明,浮游植物光吸收参数化方程中各系数存在显著的季节差异(2倍以上)。对NAP和CDOM光吸收进行了参数化处理,揭示了吸收系数和指数斜率的变化范围,并给出了它们的季节动态。NAP和CDOM吸收系数的年变化与TChl-a的年变化周期相反。浮游植物华多后,NAP和CDOM吸收系数增加,tch -a降低。浮游植物、NAP和CDOM对440 nm颗粒和溶解物总吸收的相对贡献在年内变化显著。冬季和夏季浮游植物对吸收的贡献最大,春季和秋季CDOM和NAP对吸收的贡献最大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Spectral Light Absorption Coefficient of Particles and Colored Dissolved Organic Matter in the Sea of Azov
The research was carried out based on the results of measuring the concentration of chlorophyll-a (TChl-a), spectral coefficient of light absorption by phytoplankton, non-algal particles (NAP) and colored dissolved organic matter (CDOM) in the southern part of the Sea of Azov in different seasons from 2016 to 2020. New data for the Sea of Azov on the variability of the spectral coefficient of light absorption by all optically active components have been obtained. A high (more than an order of magnitude) variability of all studied parameters was shown. The seasonal dynamics of TChl-a shows maxima in winter and summer. A relationship between the phytoplankton absorption and TChl-a has been revealed, which is described by a power function. Significant seasonal differences (two or more times) between the coefficients in the equation for parametrization of light absorption by phytoplankton were revealed. The NAP and CDOM light absorption were parametrized, the ranges of variability of the absorption coefficient and the exponential slope were revealed, and their seasonal dynamics was shown. Annual variability of absorption coefficient of NAP and CDOM was opposite to the annual cycle of TChl-a. The NAP and CDOM absorption coefficients increased after phytoplankton blooms, when TChl-a decreased. The relative contribution of phytoplankton, NAP, and CDOM to the total absorption by particles and dissolved matter at 440 nm varied significantly over the year. The share of phytoplankton was maximum in winter and summer, while in spring and autumn the maximum contribution to absorption was made by CDOM and NAP.
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