Estimation Of Pelagic Fishing Area in Banten’s Southern Sea

Andhita Rossi Pratiwi, Ririn Irnawati, M. Khalifa
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Abstract

The purpose of this research are to determine the average distribution of SST, chlorophyll-a, and see surface currents, and analyze the relationship between them with pelagic fish catches as an analysis material for determining pelagic fishing area in Banten’s Southern Sea. Data collected includes SST and chlorophyll-a using Aqua MODIS images data and and see surface currents data from Copernicus Marine Data for 6 years. The data was processed to produce the value of each parameter and then analyzed the parameters with the catches and determine the potential pelagic fishing area. The results showed that the SST throughout 2016 had a relatively high value allegedly due to the negative Indian Ocean Dipole (IOD). During the eastern until the end of second transitional season in 2019 there was a positive IOD which caused SST to decrease and chlorophyll-a to be larger than in other fishing seasons. See surface currents in the western season tend to be larger than in other fishing seasons. SST and chlorophyll-a have a stronger relationship with catches than see surface currents. The potential fishing area are around Tanjung Mantiyung, Muara Binuangeun, dan Tanjung Panto.
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万丹南部海域远洋捕捞面积估算
本研究的目的是确定万丹南海海温、叶绿素-a、表层海流的平均分布,并分析它们与中上层渔获量的关系,作为确定中上层渔区的分析资料。收集的数据包括使用Aqua MODIS图像数据的海表温度和叶绿素-a,以及使用哥白尼海洋数据收集的6年表面洋流数据。对数据进行处理,得到各参数值,并与渔获量进行分析,确定潜在的远洋捕捞区。结果表明,2016年全年的海温相对较高,可能是由于负印度洋偶极子(IOD)。东部至2019年第2个过渡季结束时存在正IOD,导致海表温度降低,叶绿素-a大于其他渔季。看,在西部季节的表面水流往往比其他捕鱼季节大。海温和叶绿素-a与渔获量的关系强于表层海流。潜在的捕鱼区在丹绒Mantiyung、Muara binuangun、丹绒Panto附近。
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