Journal of Tropical Oceanography ›› 2023, Vol. 42 ›› Issue (3): 86-95.doi: 10.11978/2022146CSTR: 32234.14.2022146

• Marine Physics • Previous Articles     Next Articles

Studying on diffuse attenuation coefficient in the South China Sea based on volume scattering function and absorption coefficient*

ZHANG Xianqing1,2(), LI Cai1,3(), Zhou Wen1,3, LIU Cong1, XU Zhantang1,3, CAO Wenxi1,3, YANG Yuezhong1,3   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. Southern Marine Science and Engineering Guangdong Laboratory, Guangzhou 511458, China
  • Received:2022-06-27 Revised:2022-08-12 Online:2023-05-10 Published:2022-08-24
  • Supported by:
    National Natural Science Foundation of China(41976181); National Natural Science Foundation of China(41976172); National Natural Science Foundation of China(41976170); Science and Technology Planning Project of Guangzhou City China(201707020023); Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0305); Open Project Program of the State Key Laboratory of Tropical Oceanography(LTOZZ1602)

Abstract:

Diffuse attenuation coefficient of downwelling irradiance Kd(z, λ) is an important parameter for estimating the profile distribution of underwater light filed and water constituents, and studying the photosynthesis of the phytoplankton and warning method of harmful algae bloom. Kd(z, λ) is a “quasi-inherent” optical property as a function of wavelength   λ and depth z. Not only is it sensitive to absorption and scattering/backscattering coefficient, but also sensitive to the angular distribution of the normalized volume scattering function (i.e., scattering phase function). In this study, based on the volume scattering function [VSF, β(ψ, z)] in seven directions determined with a custom in situ device called VSAM (volume scattering and attenuation meter), the absorption coefficient a(z) determined with the WET Labs ac9 and ac-s, and the downwelling irradiance Ed(z) determined with the Satlantic Profiler Ⅱ OCI/R-200 and HyperPro Ⅱ in the north South China Sea (SCS) with a broad range, using LightGBM, Random Forest (RF) and CatBoost, three machine learning models for estimating the profile distribution of Kd(z, 650) were developed at first, and they were then evaluated by the key indicators including R2、RMSE、MAPE, as well as the comparison between in situ measured Kd(650) and estimated Kd(650). The evaluation indicated that the CatBoost model performed the best with R2 of 0.8534, RMSE of 0.0472 m-1, MAPE of 11.0585%, and the estimated Kd(650) was also closest to the measured Kd(650). Using the established CatBoost model, input inherent optical properties (IOPs) were the absorption coefficient, the volume scattering function (VSF), and their profile depth, the Kd(650) profile distribution among 15 m in the north SCS was estimated. The result shows that Kd(650) varies from 0.275 to 0.7 m-1 at 5, 10 and 15 m underwater. At 5 m, Kd(650) is relatively stable while it varies greatly at 10 and 15 m. The contribution of volume scattering function distribution to Kd(z, λ) is considered in this study, which provides a new idea and method for accurate estimation and acquisition of Kd(z, λ) based on inherent optical properties (IOPs).

Key words: diffuse attenuation coefficient Kd(650), volume scattering function, absorption coefficient, machine learning