塞内加尔专属经济区海表温度和叶绿素浓度的季节变化及其与远洋鱼类捕捞的相关性

J. M. Kouadio, W. Ndiaye, Ahon Jean-Baptiste Kassi, Tacko Niang, É. Djagoua, A. Diouf
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引用次数: 0

摘要

本研究利用遥感数据分析了2003年至2017年塞内加尔专属经济区(EEZ)海洋生物物理特征及其与沿海中上层鱼类捕捞的关系。采用3级(4 km)月海表温度(SST)、MODIS-Aqua中分辨率成像光谱仪卫星(MODIS-Aqua)叶绿素(Chl-a)数据和统计渔业数据。这些与沿海上升流指数和湍流水指数相关的生物物理参数可以表征鱼类的可用性。生物物理参数的月平均变化表明,叶绿素浓度、海面温度和浮游生物可利用性之间存在密切的关系。结果表明,高叶绿素a浓度和高上升流强度与低海表温度有直接关系。年际变化分析显示出两个明显的季节特征。从11月到5月的寒冷季节,以强烈的上升流为特征,对应于高浓度的叶绿素和高上升流强度,沿海远洋物种的登陆量非常高。6 - 10月为暖季,叶绿素浓度低,上升流强度减弱,登陆值低。6 ~ 10月为炎热季节,叶绿素- A浓度较低,上升流强度减弱,登陆值较低。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal Variability of Sea Surface Temperature and Chlorophyll Concentration and Its Correlation with Pelagic Fish Catch in Senegalese Exclusive Economic Zone (EEZ)
Remote sensing data were used in this study to relate the biophysical characteristics of the ocean and their relationship with the coastal pelagic fish catches in the Senegalese Exclusive Economic Zone (EEZ) from 2003 to 2017. Level 3 (4 km) monthly sea surface temperature (SST), chlorophyll (Chl-a) data from the Moderate Resolution Imaging Spectroradiometer Satellite (MODIS-Aqua) and statistics fishing data were used. These biophysical parameters associated to coastal upwelling index and turbulence water index allowed to characterise availability of fish. The monthly average variation of the biophysical parameters shows a close relation between chlorophyll concentration, sea surface temperature and the pelagic species availability. The results showed that satellite variables are directly related, with high chlorophyll-a concentrations and high upwelling intensities corresponding to low ocean surface temperature. The analysis of intra-annual variations shows the identification of two distinct seasons. A cold season from November to May, marked by an intense upwelling, corresponding to a high concentration of chlorophyll and high upwelling intensity with very high landings of coastal pelagic species. A warm season from June to October corresponding to a low concentration of chlorophyll and a decrease in the intensity of upwelling with low landing values. A hot season extending from June to October, corresponds to a low concentration of chlorophyll-a and a decrease in intensity of upwelling with low landing values.
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