scholarly journals Winter distribution of young walleye pollock Theragra chalcogramma investigated with quantitative echosounder on the Pacific coast of eastern Hokkaido, Japan

2008 ◽  
Vol 74 (2) ◽  
pp. 152-160 ◽  
Author(s):  
OSAMU SHIDA ◽  
HIROYA MIYAKE ◽  
TOMONORI KANETA ◽  
RYOTARO ISHIDA ◽  
KAZUSHI MIYASHITA
2021 ◽  
Vol 201 (2) ◽  
pp. 340-358
Author(s):  
S. L. Ovsyannikova ◽  
E. E. Ovsyannikov ◽  
Yu. V. Novikov

Data on spatial distribution and habitat conditions are presented for walleye pollock Theragra chalcogramma at southern Kuril Islands in spawning season (spring 2015) and feeding season (summer 2016). In spring, walleye pollock are distributed over the entire shelf and continental slope down to 900 m depth and occupy the upper layer on the shelf and intermediate layer at the slope with water temperature 0.1–1.5 o C. In summer, they aggregate at the depth of 200–270 m beyond the shelf in the intermediate water at the Pacific slope of Iturup Island, under the temperature of 1.3–2.9 o C. Both spatial and bathymetric migrations of pollock are minimal at the Pacific side of Iturup, but they migrate for spawning westward and southwestward to the Okhotsk Sea and slope of Small Kuril Ridge where concentrate at the benthic front between the tidal mixing zone and the Intermediate water. Seasonal redistribution of walleye pollock is accompanied with changes of size-age structure in the main aggregations.


2013 ◽  
Vol 70 (6) ◽  
pp. 1162-1173 ◽  
Author(s):  
Steven J. Barbeaux ◽  
John K. Horne ◽  
Martin W. Dorn

Abstract Barbeaux, S. J., Horne, J. K., and Dorn, M. W. 2013. Characterizing walleye pollock (Theragra chalcogramma) winter distribution from opportunistic acoustic data. – ICES Journal of Marine Science, 70: 1162–1173. In 2003, acoustic data from 25 000 km of ship track lines were collected from two fishing vessels participating in the eastern Bering Sea walleye pollock (Theragra chalcogramma) fishery. Although these data were not calibrated or collected on a systematic grid, their broad temporal extent combined with high spatial resolution facilitated the examination of the distribution and behaviour of fished aggregations. To demonstrate their scientific applicability, these data were used to identify the spatio-temporal dynamics of pollock aggregations over scales ranging from hundreds of metres to hundreds of kilometres and from minutes to months. The spatial analysis identified three levels of pollock aggregation. The largest regions of high pollock density had an average diameter of 110 km and were comparable with distinct fishing grounds identified by fishers. The next smaller areas of high pollock density had a diameter between 2.5 and 6 km. Within these areas were clusters of pollock at even higher densities. The extent of the smallest aggregations ranged in diameter from 0.1 km in daylight to 0.6 km at night. Time-series analysis identified vertical and horizontal diel changes in pollock distribution and an overall decline in pollock density over the study period.


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