论文

西北太平洋柔鱼中心渔场分布模式

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  • 中国科学院地理科学与资源研究所,北京100101
邵全琴(1962-),女,江苏武进人,研究员,博士生导师。研究方向为海洋GIS。shaoqq@lreis.ac.cn

收稿日期: 2003-07-08

  修回日期: 2003-11-24

  网络出版日期: 2004-02-15

基金资助

中国科学院知识创新工程资助项目(CX10GD0010);国家863计划资助项目(8638181103)

Study on spatial patterns of Ommastrephes Bartrami Fishing Ground in the Northwest Pacific Ocean

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  • Institute of Geographic Sciences and Natural Resources Research, CAS, Beijing 100101,China

Received date: 2003-07-08

  Revised date: 2003-11-24

  Online published: 2004-02-15

摘要

本文利用ArcGIS对西北太平洋SST和柔鱼渔捞统计时间序列数据进行了处理分析 ,研究了西北太平洋柔鱼中心渔场分布模式。该海域柔鱼中心渔场有三类 :舌型渔场、枝叉型渔场、涡流型渔场。涡流型渔场出现次数最高、渔获总产量最高、CPUE平均值最高 ,表层水温为 10~ 18℃。舌型渔场出现次数第二、渔获总产量第二、CPUE平均值最低 ,表层水温为 15~2 1℃。枝叉型渔场出现次数最少、渔获总产量最低、CPUE平均值第二 ,表层水温为 17~2 4℃。 8月枝叉型渔场为主 ,9月舌型渔场为主 ,10月舌型渔场和涡流型渔场为主 ,11月涡流型渔场为主。

本文引用格式

邵全琴, 戎恺, 马巍巍, 王文宇, 游智敏 . 西北太平洋柔鱼中心渔场分布模式[J]. 地理研究, 2004 , 23(1) : 1 -9 . DOI: 10.11821/yj2004010001

Abstract

This article focuses on the analysis of the relationship between Ommastrephes bartramifishing ground and marine environmental factors. Based on daily catch data of Ommastrephes bartrami during 1995 to 2000 by China fishing boats and SST isoline chart covering 1995 to 2000 issued every 3 days by Japan Fisher Information Service Center. ArcGIS was used to store, manage and analyze the data. All the catch data were processed and spatialized to display their spatial distribution. The fishing grounds were identified interactively from the catch data maps. Matching Ommastrephes bartrami fishing ground with SST isoline map revealed that the relationship between them could be divided into 3 main patterns and 16 subclasses. The fishing ground in patternⅠis distributed on the tongue of Kuroshio and Oyashio branches, hence called as tongue type. PatternⅠcan be further classified into 5 subclasses,i.e., warm tongue type, cold tongue type, warm tongue + cold tongue type, warm tongue + cold tongue+ warm tongue type, and warm tongue + cold tongue+ warm tongue + cold tongue type. PatternⅡis located on the branch of Kuroshio or Oyashio, so called as branch type. In patternⅡ, five subclasses can be defined,i.e., warm branch type, warm branch + cold tongue type, warm branch + cold tongue+ warm branch type, cold tongue+ warm branch + cold tongue type, and warm tongue+ cold branch. Pattern Ⅲ is distributed on eddy caused by Kuroshio branch encountering Oyashio branch, also named as eddy type. Pattern Ⅲ can be ulteriorly classified as warm eddy type, warm eddy + cold tongue + warm eddy type, warm eddy + cold tongue (branch) + warm tongue type, warm eddy + cold tongue type,warm eddy + cold tongue + warm branch + cold tongue + warm branch type,and warm eddy + cold tongue + warm branch type. Statistical analyses of 239 samples indicate that pattern III has the highest occurrence frequency and highest catch, and pattern II has the lowest occurrence and lowest production. Subclass 35 has the highest occurrence frequency, and subclass 14 has the highest catch. The average CPUE of pattern Ⅲ is the highest, patternⅠthe lowest.Subclass 31 has the highest CPUE value. In 1995 and 1996, patternsⅡ and Ⅲ dominate. In 1997, pattern Ⅲ dominates. From 1998 to 2000, patternⅠis in domination. In August, patternⅡis in domination. In September, patternⅠdominates. In October, patternsⅠand Ⅲ are in domination. In November, patternⅢ dominates. The SST in patternⅠ usually falls between 15℃and 21℃,patternⅡ,17~24℃, and patternⅢ,10~18℃. The temperature grade in the patternⅠchanges slowly, while pattern Ⅲ, has a big grade change. PatternⅠis mainly located on Kurushio branches 3 and 4, patternⅡon Kurushio branches 2 and 3,and pattern Ⅲ mainly located on Kurushio branches 1 and 2.

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