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Distribution of the Soviet krill fishing fleet in the South Orkneys area (Subarea 48.2) during 1989/90

机译:1989/90年期间,苏联磷虾捕捞船队在南奥克尼地区(分区48.2)的分布

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The results of an analysis of haul-by-haul catch statistics from the Soviet krill fishing fleet during the 1989/90 season (sample of 3 614 hauls for the period from 1 November 1989 to 12 June 1990) are presented. During the season, fishing vessels worked one fishing ground off the northwestern tip of Coronation Island. CPUE showed variability with a minimum in November (3.2 tonnes/hour) and maximums in February and March (9.6 tonnes/hour and 11.0 tonnes/hour respectively), followed by a decrease to 6.9 and 7.1 tonnes/hour by May and June. The location of the fishing ground was observed to be stable, and it is considered that the location was determined by certain hydrodynamic characteristics of the area, for example a complex current around the islands together with topographically-induced effects. Except in November 1989, temporally and spatially sustained fishable krill aggregations did not form outside the main fishing area. During the November period the commercial fleet fished over oceanic areas, and targeted krill aggregations found in the major current flowing towards the north-east of the region. The fleet was observed drifting with the current together with krill aggregations. A maximum CPUE (3.8 tonnes/hour) was recorded at the beginning of the period, with a subsequent gradual decrease towards the minimum level acceptable to the fleet (2.5 tonnes/hour). Over the last five days of November, the aggregation disintegrated, having existed for about 25 days, and commercial vessels returned to Coronation Island. Krill drift velocity, estimated on the basis of the fishing ground shift, amounted to 7.4 km/day or 8.7 cm/sec. This is comparable to, though less than, the drift velocity off Elephant Island (11 to 13 cm/sec), evaluated earlier using the same method (Sushin and Myskov, 1992).
机译:列出了1989/90年度苏联磷虾捕捞船队逐个批次捕获统计数据的分析结果(1989年11月1日至1990年6月12日期间3 614批次的样本)。在本季节中,渔船在加冕岛西北端附近的一个渔场工作。 CPUE表现出可变性,11月最低(3.2吨/小时),2月和3月最高(分别为9.6吨/小时和11.0吨/小时),然后到5月和6月分别降至6.9吨和7.1吨/小时。观察到渔场的位置是稳定的,并且认为该位置是由该区域的某些水动力特性确定的,例如,岛屿周围的复杂水流以及地形诱发的影响。除1989年11月外,在主要捕捞区域以外没有形成时空可持续的可捕磷虾聚集体。在11月期间,商业船队在大洋区域捕鱼,在流向该地区东北部的主要水流中发现了有针对性的磷虾聚集体。观察到舰队随着海流和磷虾的聚集而漂移。在此期间开始时记录了最大CPUE(3.8吨/小时),随后逐渐降低到机队可接受的最小水平(2.5吨/小时)。在11月的最后五天中,聚集体解体了,已经存在了约25天,商业船只返回加冕岛。磷虾漂移速度是根据渔场的变化估算的,为7.4 km /天或8.7 cm / sec。这与早期使用相同方法评估的象岛(11至13厘米/秒)的漂移速度相当,但小于(Sushin和Myskov,1992)。

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