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西北太平洋柔鱼渔场分布与涡动能变化的相关关系

刘瑜 郑全安 李晓峰

刘瑜,郑全安,李晓峰. 西北太平洋柔鱼渔场分布与涡动能变化的相关关系[J]. 海洋学报,2020,42(2):44–51,doi:10.3969/j.issn.0253−4193.2020.02.005
引用本文: 刘瑜,郑全安,李晓峰. 西北太平洋柔鱼渔场分布与涡动能变化的相关关系[J]. 海洋学报,2020,42(2):44–51,doi:10.3969/j.issn. 0253−4193.2020.02.005
Liu Yu,Zheng Quanan,Li Xiaofeng. Relationship between neon flying squid Ommastrephes bartramii fishery distribution patterns and eddy kinetic energy in Northwest Pacific Ocean[J]. Haiyang Xuebao,2020, 42(2):44–51,doi:10.3969/j.issn.0253−4193.2020.02.005
Citation: Liu Yu,Zheng Quanan,Li Xiaofeng. Relationship between neon flying squid Ommastrephes bartramii fishery distribution patterns and eddy kinetic energy in Northwest Pacific Ocean[J]. Haiyang Xuebao,2020, 42(2):44–51,doi:10.3969/j.issn.0253−4193.2020.02.005

西北太平洋柔鱼渔场分布与涡动能变化的相关关系

doi: 10.3969/j.issn.0253-4193.2020.02.005
基金项目: “十二五”国家科技支撑计划“大洋性渔业捕捞技术与新资源开发”(2013BAD13B05)。
详细信息
    作者简介:

    刘瑜(1985—),女,山东省烟台市人,工程师,主要研究方向为渔业遥感。E-mail:liuy@shou.edu.cn

    通讯作者:

    李晓峰,教授,主要从事海洋遥感和人工智能海洋研究。E-mail:xfli@shou.edu.cn

  • 中图分类号: P745

Relationship between neon flying squid Ommastrephes bartramii fishery distribution patterns and eddy kinetic energy in Northwest Pacific Ocean

  • 摘要: 本研究利用卫星高度计数据计算海洋涡动能(Eddy Kinetic Energy,EKE),根据2010–2016年中国远洋渔业协会鱿钓组提供的西北太平洋柔鱼(Ommastrephes bartramii)渔业生产数据,分析柔鱼渔场的EKE分布特征以及黑潮延伸体EKE的时空变化对柔鱼渔场分布的影响。结果显示,柔鱼渔场的EKE与单位捕捞努力量渔获量(Catch Per Unit Effort,CPUE)呈显著负相关(P < 0.01),EKE对CPUE的有效影响范围为0~1 500 cm2/s2,最适宜EKE范围为25~150 cm2/s2。黑潮延伸体EKE强度由西向东递减,与CPUE年平均呈负相关,相关系数为0.81(P < 0.05)。按黑潮延伸体经度范围分为4个子区域,CPUE月平均纬度重心响应该月EKE强度最高的子区域。盛渔期8–10月渔场距离黑潮延伸体在800~1 000 km范围内时,CPUE随距离增加而增大,其中最适宜的距离范围为850~950 km。研究表明,当黑潮延伸体路径弯曲多变时,EKE增大,而柔鱼CPUE变低,渔场位置越偏北。
  • 图  1  研究区域和渔场重心位置(黄色圆圈)

    Fig.  1  Study area and the locations of fishing ground centroids (yellow circles)

    图  2  2010−2016年7−11月柔鱼的月平均CPUE和EKE变化

    Fig.  2  Variations of the monthly average CPUE and EKE from July to November during 2010−2016

    图  3  2010−2016年7−11月CPUE在各EKE区间内的累积频率分布

    Fig.  3  Distribution of CPUE frequencies in relation to EKE from July to November during 2010−2016

    图  4  EKE与CPUE关系的GAM分析图

    S为光滑样条函数的拟合值,表示其对CPUE的影响。虚线表示 95% 的置信区间,实线表示拟合后平均值

    Fig.  4  GAM analysis of the relationship between EKE and CPUE

    S is the fitted value of smoothing spline functions, which represent their impacts on CPUE. Dashed lines indicate 95% confidence intervals, solid line indicates the mean of fitted data

    图  5  2010−2016年7−11月CPUE与黑潮延伸体EKE_A相关变化图

    虚线表示每年的平均值,实线表示拟合后平均值

    Fig.  5  Variations of the monthly average CPUE and EKE_A of the Kuroshio Extension from July to November during 2010−2016

    Dashed lines indicate the average of each year, solid line indicates the mean of fitted data

    图  6  2010−2016年7−11月黑潮延伸体各子区域的EKE变化

    Fig.  6  Variations of the EKE in sub-areas of the Kuroshio Extension from July to November during 2010−2016

    图  7  2010−2016年7−11月CPUE渔场分布重心变化

    Fig.  7  Fishing ground centroids from July to November, 2010−2016

    图  8  不同区域DIST与CPUE关系的GAM分析

    Fig.  8  GAM analysis of the relationship between DIST of sub-areas and CPUE

    图  9  2013−2015年8−10月渔场重心与月平均EKE分布图(黄色圆圈表示渔场重心)

    Fig.  9  Maps of fishing ground centroids (yellow circles) with backgrounds of monthly average EKE from August to October, 2013−2015

    表  1  CPUE纬度重心与黑潮延伸体EKE的相关关系

    Tab.  1  Correlations of the latitudinal centroids of CPUE to EKE of the Kuroshio Extension

    年/份7月8月9月10月11月
    20100.77_D0.79_BP>0.050.69_DP>0.05
    20110.55_E0.91_BP>0.050.85_CP>0.05
    20120.81_D0.71_B0.91_E0.82_CP>0.05
    20130.86_D0.96_BP>0.050.70_CP>0.05
    20140.51_E0.87_C0.86_C0.83_CP>0.05
    20150.84_E0.73_B0.36_CP>0.05P>0.05
    20160.74_D0.82_B0.60_CP>0.05P>0.05
      注:表中有系数值时均为P < 0.01;_B、C、D、E表示子区域。
    下载: 导出CSV
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出版历程
  • 收稿日期:  2019-01-06
  • 修回日期:  2019-05-10
  • 网络出版日期:  2020-11-18
  • 刊出日期:  2020-02-25

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