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2008年夏季南海北部海区生物光学特性的垂向变化特征
引用本文:王桂芬,周雯,许占堂,徐文龙,杨跃忠,曹文熙.2008年夏季南海北部海区生物光学特性的垂向变化特征[J].海洋学报(英文版),2020,39(4):42-56.
作者姓名:王桂芬  周雯  许占堂  徐文龙  杨跃忠  曹文熙
作者单位:河海大学 海洋学院, 中国 南京 210098;热带海洋环境国家重点实验室, 中国科学院南海海洋研究所, 中国 广州 510301
基金项目:The National Natural Science Foundation of China under contract Nos 41776045 and 41576030; the Fundamental Research Funds for the Central Universities under contract No. 2017B06714; the Open Project Program of the State Key Laboratory of Tropical Oceanography under contract No. LTOZZ1602; the Science and Technology Program of Guangzhou, China under contract No. 201607020041.
摘    要:Vertical variability in the bio-optical properties of seawater in the northern South China Sea(NSCS) including inherent optical properties(IOPs) and chlorophyll a concentration(Chl) were studied on the basis of in situ data collected in summer 2008 using an absorption/attenuation spectrophotometer. An empirical model was developed to estimate Chl profiles based on the absorption line height at long wavelengths, with a relative root mean square error of 37.03%. Bio-optical properties exhibited large horizontal and vertical spatial variability. As influenced by coastal upwelling and the Zhujiang River(Pearl River) discharge, both IOPs and Chl exhibited high values in the surface waters of the inner shelf, which tended to decrease with distance offshore. Subsurface maximum layers of IOPs and Chl were observed in the middle and outer shelf regions, along with significantly higher values of attenuation coefficients beneath this layer that rapidly increased towards the bottom. In the open ocean, both IOPs and Chl exhibited consistent variability, with the subsurface maximum layer typically located at34–84 m. Phytoplankton were found to be one of the major components in determining the vertical variability of bio-optical properties, with their vertical dynamics influenced by both physical forcing and light attenuation effects. The depth of the subsurface maximum layer was found to be closely related to the fluctuation of the oceanic thermocline and the depth of the euphotic zone, which also affected the total integrated biomass of the upper ocean. Typically high values of attenuation coefficients observed in the bottom waters of the continental shelf reflected the transport of particulate matter over the bottom boundary layer. Our results reveal large spatial differences in bio-optical profiles in response to complex marine ecodynamics in the NSCS. From the perspective of marine research, high-resolution optical measurements are clearly advantageous over conventional bottle sampling.

关 键 词:垂向分布  浮游植物  生物光学特性  次表层叶绿素最大值层  南海北部海区
收稿时间:2019/1/28 0:00:00

Vertical variations in the bio-optical properties of seawater in the northern South China Sea during summer 2008
Wang Guifen,Zhou Wen,Xu Zhantang,Xu Wenlong,Yang Yuezhong,Cao Wenxi.Vertical variations in the bio-optical properties of seawater in the northern South China Sea during summer 2008[J].Acta Oceanologica Sinica,2020,39(4):42-56.
Authors:Wang Guifen  Zhou Wen  Xu Zhantang  Xu Wenlong  Yang Yuezhong  Cao Wenxi
Institution:1.College of Oceanography, Hohai University, Nanjing 210098, China2.State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
Abstract:Vertical variability in the bio-optical properties of seawater in the northern South China Sea (NSCS) including inherent optical properties (IOPs) and chlorophyll a concentration (Chl) were studied on the basis of in situ data collected in summer 2008 using an absorption/attenuation spectrophotometer. An empirical model was developed to estimate Chl profiles based on the absorption line height at long wavelengths, with a relative root mean square error of 37.03%. Bio-optical properties exhibited large horizontal and vertical spatial variability. As influenced by coastal upwelling and the Zhujiang River (Pearl River) discharge, both IOPs and Chl exhibited high values in the surface waters of the inner shelf, which tended to decrease with distance offshore. Subsurface maximum layers of IOPs and Chl were observed in the middle and outer shelf regions, along with significantly higher values of attenuation coefficients beneath this layer that rapidly increased towards the bottom. In the open ocean, both IOPs and Chl exhibited consistent variability, with the subsurface maximum layer typically located at 34–84 m. Phytoplankton were found to be one of the major components in determining the vertical variability of bio-optical properties, with their vertical dynamics influenced by both physical forcing and light attenuation effects. The depth of the subsurface maximum layer was found to be closely related to the fluctuation of the oceanic thermocline and the depth of the euphotic zone, which also affected the total integrated biomass of the upper ocean. Typically high values of attenuation coefficients observed in the bottom waters of the continental shelf reflected the transport of particulate matter over the bottom boundary layer. Our results reveal large spatial differences in bio-optical profiles in response to complex marine ecodynamics in the NSCS. From the perspective of marine research, high-resolution optical measurements are clearly advantageous over conventional bottle sampling.
Keywords:vertical distribution  phytoplankton  bio-optical properties  subsurface maximum layer  northern South China Sea
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