期刊
ICES JOURNAL OF MARINE SCIENCE
卷 63, 期 8, 页码 1465-1476出版社
OXFORD UNIV PRESS
DOI: 10.1016/j.icesjms.2006.06.007
关键词
age identification; common observation range; morphology and bathymetry; optimal size of an integration cell; pattern of Delta MVBS
The purpose of this study was to investigate the possibility of identifying the age of walleye Pollock (Theragra chalcogramma) using acoustic information. Acoustic data targeting walleye pollock were collected at 38 and 120 kHz from 16 June to 12 July 2000 in the Pacific, off Hokkaido, Japan. To complement these data 33 trawl hauls were made and the species and age of the sample fish were accurately examined. The echoes of walleye pollock schools according to age were used to determine the morphological and bathymetric characteristics such as mean height, maximum length, centre depth, seabed depth, and distance from the seabed, as well as the frequency characteristics, this latter being the difference of mean volume backscattering strengths at 38 and 120 kHz, respectively (Delta MVBS). The Delta MVBS method is elaborated using MVBS (mean volume backscattering strength) from an integration cell of optimal size, the cell being examined by means of various integration periods to highlight the characteristics of the walleye pollock schools resulting in 20 pings (120 m), and by applying this method only in a common observation range for two frequencies. The ages of the schools are identified by a combination of morphological and bathymetric characteristics, and Delta MVBS characteristics. Age-0 groups are easy to distinguish from other age groups because they exist in distinct, small schools, are close to the coast, and have a narrow range of Delta MVBS regardless of time of day. Age-1 schools are low in height and very long, are distributed close to the sea floor, and have an Delta MVBS range of -1 to 8 dB, with most between 3 and 5 dB. These characteristics of age-1 schools are distinct from other age groups. As age-2 and age-5 schools have similar maximum length and distribution depth, it is almost impossible to identify these two by just morphological and bathymetric characteristics. However, the AMVBS of age-2 and age-5 schools show characteristic patterns that can be used as a means of identification. The pattern of Delta MVBS, which reflects an internal structure (swimming angles) of a school, is different for each age class, and is essential in the identification of the age of a walleye Pollock school. (c) 2006 International Council for the Exploration of the Sea. Published by Elsevier Ltd. All rights reserved.
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