基于栖息地模型的西北太平洋柔鱼索饵洄游路径推测及其与厄尔尼诺-南方涛动的关系

Prediction of the migration route of Ommastrephes bartramii in Northwest Pacific Ocean based on Habitat Suitability Model and its relationship with ENSO

  • 摘要:
    目的 为了探明西北太平洋柔鱼索饵洄游的一般路径。
    方法 采用海表温度(SST)、海表高度(SSH)和光合有效辐射(PAR)等环境数据和生产统计数据建立栖息地适宜性模型(HSI ),分析1998—2020年7—11月索饵期间柔鱼洄游分布及其与尼尔尼诺-南方涛动(ENSO)的关系。
    结果 7月上旬柔鱼广泛分布于152~165° E,38~42° N海域,在索饵洄游的第一阶段,柔鱼快速朝着西北方向聚集并于8月上旬行至155.48°E,41.75°N;第二阶段,沿着亚北极峰转向北偏东方向缓慢移动,9月下旬到达洄游最北端(156.56°E,43.46°N);第三阶段,开始逐步朝西南方向径直返回,11月下旬抵达151.52°E,41.26°N。过去的23年里,柔鱼洄游路径年际差异显著,经度偏移值约为1.7°,纬度偏移值约为0.5°。研究发现,ENSO事件会影响柔鱼幼体的时空分布,致使北上索饵过程更偏向东;与正常年份相比,拉尼娜发生时,柔鱼因适宜生境扩大而快速生长,向北迁徙速度更快,最北端纬度更高(43.76° N);而厄尔尼诺年则相反,洄游将滞留在43° N以南,南北迁徙相对缓慢,且受区域环境约束,在8月中旬至10月上旬趋于聚集,有利于商业捕捞。
    结论 西北太平洋柔鱼索饵洄游存在既定的路线,能对ENSO事件产生独特的响应。本研究为西北太平洋柔鱼资源的科学认知提供了支撑。

     

    Abstract: The environmentally sensitive neon flying squid (Ommastrephes bartramii) undertakes large-scale, long-range and seasonal migrations between spawning and feeding grounds in the Northwest Pacific to seek the optimal habitat conditions for growth and development. To elucidate the general feeding migration routes of the neon flying squid in the Northwest Pacific Ocean, this study developed a Habitat Suitability Index (HSI) model utilizing environmental data, including Sea Surface Temperature (SST), Sea Surface Height (SSH), and Photosynthetically Active Radiation (PAR), along with fisheries catch statistics. The model was applied to analyze the squid's migration distribution during the feeding season (from July to November) from 1998 to 2020 and its relationship with the El Niño Southern Oscillation (ENSO). The results indicated that in early July, the squid were widely distributed within 152°–165°E and 38°–42°N. The feeding migration comprised three distinct phases: 1) Initially, the squid aggregated rapidly northwestward, reaching 155.48°E, 41.75°N by early August. 2) Subsequently, they turned northeastward, progressed slowly along the Subarctic Front, and arrived at the northernmost point (156.56°E, 43.46°N) in late September. 3) Finally, they commenced a direct return migration southwestward, arriving at 151.52°E, 41.26°N by late November. Over the past 23 years, the significant interannual variability was observed in the migration routes, with longitudinal and latitudinal shifts of approximately 1.7° and 0.5°, respectively. The research reveals that ENSO events influence the spatiotemporal distribution of juvenile squid, leading to a more eastward-biased northward feeding migration. Compared to normal years, during La Niña events, the expanded suitable habitat promoted faster growth and a quicker northward migration, resulting in a more northerly terminus (43.76°N). Conversely, during El Niño years, the migration tended to stall south of 43°N, with slower north-south progression. Furthermore, constrained by regional environmental conditions, the squid exhibited a higher aggregation tendency from mid-August to early October, which enhanced the commercial fishing efficiency. It is concluded that the neon flying squid in the Northwest Pacific follows a defined feeding migration route, which exists distinct modifications in response to ENSO events. These findings particularly provide a scientific support for understanding and managing the fisheries resource of neon flying squid in the Northwest Pacific Ocean.

     

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