首页> 外文会议>Proceedings of the 22nd Asian Conference on Remote Sensing >DELINEATION OF MESO SCALE FEATURES IN THE KUROSHIO-OYASHIO TRANSITION REGION AND FISH MIGRATION ROUTES USING SATELLITE DATA OFF JAPAN
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DELINEATION OF MESO SCALE FEATURES IN THE KUROSHIO-OYASHIO TRANSITION REGION AND FISH MIGRATION ROUTES USING SATELLITE DATA OFF JAPAN

机译:利用日本以外的卫星资料划定黑潮-大矢尾过渡区中尺度特征和鱼类迁徙路线

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Kuroshio warm-core rings (KWCR) are invariably formed from the intensification of Kuroshio Extension transport heat, salt and biomass from lower to higher latitudes. The distribution pattern of these rings and other meso-scale features such as eddies, cold and warm streamers in Kuroshio-Oyashio transition region and their interaction results in the occurrence and migration of potential fisheries zones (PFZ). Past studies have shown that formation of fishery grounds and their migration attribute to warm and cold streamers entrained along the periphery of warm-core rings. In this paper combining NOAA-AVHRR, ADEOS/OCTS data and sea truth observations, we describe different meso-scale features and their interactions with surrounding water through local advection and streamer activities as well as how fish species utilize different range of temperatures and phytoplankton blooming areas for their migration. It is noteworthy that sardine schools use the warm streamers for their migration towards north from Kuroshio Extension to warm-core rings and from the warm-core rings to the coastal waters within a specific range of thermal and chlorophyll signature. Similarly, skipjack moves in a range of temperature (20.5 - 23.0°C) and pigment concentration (0.12-0.16 μg/l) in the Kuroshio region. The movement of fishing grounds associated with the warm-core rings and warm streamers are also discussed. It is concluded that the satellite information provides a space/time overview of different oceanographic features can profitably be utilized in delineating PFZ and increases our understanding how they are continually interacting.
机译:黑潮暖心环(KWCR)始终是由黑潮扩展从低纬度到高纬度的热,盐和生物质的强化而形成的。这些环和其他中尺度特征的分布模式,如黑潮—大潮过渡区中的涡流,冷,暖流光及其相互作用,导致了潜在渔业区(PFZ)的发生和迁移。过去的研究表明,渔场的形成和它们的迁移归因于沿暖芯环外围夹带的温暖和寒冷的飘带。在本文中,结合NOAA-AVHRR,ADEOS / OCTS数据和海洋真相观测,我们描述了不同的中尺度特征及其通过局部对流和流光活动与周围水域的相互作用,以及鱼类如何利用不同温度范围和浮游植物的开花他们的迁移地区。值得注意的是,沙丁鱼学校使用温暖的彩带在一定范围的热和叶绿素特征范围内从黑潮延伸区向北向暖芯环以及从暖芯环向沿海水域迁移。同样,skip鱼在黑潮地区的温度(20.5-23.0°C)和颜料浓度(0.12-0.16μg/ l)范围内移动。还讨论了与暖芯环和暖彩带有关的渔场的运动。结论是,卫星信息提供了不同海洋特征的时空概况,可用于划定PFZ并有益于我们了解它们如何不断相互作用。

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