Inversion model of diatom concentrations in coastal water based on absorption coefficients

FAN Jie; SUN Deyong; WANG Shengqiang; ZHANG Hailong; HUAN Yu; HE Yijun

doi:10.11834/jrs.20210475

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Inversion model of diatom concentrations in coastal water based on absorption coefficients
Vol. 27, Issue 2, Pages: 363-375(2023)
Received：11 November 2020，

Published：07 February 2023
DOI： 10.11834/jrs.20210475
稿件说明：

移动端阅览

樊杰，孙德勇，王胜强，张海龙，环宇，何宜军.2023.结合光吸收的近海水体硅藻浓度反演模型构建.遥感学报，27（2）： 363-375 DOI： 10.11834/jrs.20210475.

Fan J，Sun D Y，Wang S Q，Zhang H L，Huan Y and He Y J. 2023. Inversion model of diatom concentrations in coastal water based on absorption coefficients. National Remote Sensing Bulletin， 27（2）：363-375 DOI： 10.11834/jrs.20210475.

摘要

浮游植物种群结构对了解海洋碳循环，生物多样性等研究具有重要意义。针对某种浮游植物种群生物量的研究，可以掌握浮游植物种群结构变化特征。本研究基于航次实测色素数据，利用CHEMTAX方法获取近海水体硅藻浓度信息，分析实测硅藻浓度数据的空间分布状态。对高斯模型中心波长和半波宽参数进行优化，结合高斯模型分解获取的高斯峰值，分析其与硅藻浓度之间的相关关系，并遴选相关系数较高的高斯峰值。利用不同数学函数，开展高斯峰值与硅藻浓度之间的关系模型构建研究，并结合精度指标（决定系数

，中值误差ME）判定各数学函数模型的硅藻浓度反演精度，以提出最优的反演模型。研究结果表明：（1）实测硅藻浓度整体上呈现出近岸高，离岸低的空间分布特征，高值区域主要分布在渤海湾及长江口附近；（2）硅藻浓度反演模型精度较高，通过留一交叉验证法对模型进行验证，决定系数为0.79，中值误差为49%，

值小于0.001，该模型为后续开展卫星遥感反演硅藻浓度的工作奠定了基础。

Abstract

Phytoplankton are a vital component of marine organisms and play a crucial role in material circulation

energy flow and information transmission. The study of phytoplankton communities is important to understand carbon cycling and biodiversity

and the study of the biomass for a certain phytoplankton group can help understand the structural changes of phytoplankton communities. Diatoms are the dominant taxonomic group with the most abundant concentration in coastal water

and diatoms provide solid photosynthetic capacity (approximately 40% of marine primary productivity). Meanwhile

diatom concentrations will indirectly affect the breeding progress of holoplankton. In this study

observation samples (

= 252) were collected in the marginal seas of the northwest Pacific Ocean

covering the Bohai Sea (BS)

Yellow Sea (YS)

and East China Sea (ECS)

from six cruise surveys that covered different seasons. The concentration of diatoms was calculated by phytoplankton pigment concentrations collected with the High-Performance Liquid Chromatography (HPLC) method with the CHEMTAX method

and the spatial distribution of measured diatom concentrations was analyzed. Based on

in situ

data parameters collected by multiple cruises

including phytoplankton absorption coefficients and diatom concentrations

we optimized Gaussian central bands and half-wave widths with derivative spectrum analysis and the peaks of the specific absorption spectrum

which were mentioned in existing research. Then

the correlation coefficients between diatom concentrations and different Gaussian peaks

which were decomposed by Gaussian function

were analyzed. We established Gaussian peaks

which had higher correlation coefficients with diatom concentrations

to establish an inversion model of diatom concentrations. The inversion models between Gaussian peaks and diatom concentrations were studied with different mathematical functions (linear function

quadratic function

logarithmic function

exponential function and power function)

and the accuracy for each model was evaluated by two precision indicators (determination coefficients

and median percent error

ME) to propose the optimal inversion model form. The parameters (

) were confirmed by leave-one-out methods later. The results of the research show the following: (1) The spatial distribution of measured diatom concentrations presented characteristics that were higher nearshore and lower offshore. The higher areas for BS appeared in the neighborhood

and the trend to the central area was decreasing progressively. Similar to BS

the spatial distribution of measured diatom concentrations was higher nearshore (Yangtze Estuary) and lower offshore (central area) in both the YS and ECS. (2) The evaluation indicators for our diatom concentration inversion model were relatively high. Comparing the diatom concentrations modeled in this study and calculated by the CHEMTAX method and using leave-one-out methods to verify the accuracy between them

the determination coefficient (

) was 0.79

the Median Error (ME) was 49%

and the

value was under 0.001. It should be noted that some deviation appears in the lower concentration (

0.02 mg m

-3

); that is why the range of application should be concluded in later applications. In summary

the relatively high accuracy shows the applicability of the inversion model of diatom concentrations in this study

and the model lays the foundation for conducting research on satellite remote sensing inversion of diatom concentrations.

关键词

Keywords

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