Abstract

Acoustic survey for density and biomass estimate of Antarctic krill, Euphausia superba, was conducted in the large area between South Shetland Islands and South Orkney Islands, during November 30-December 30, 2002. Considering oceanographic and geographic properties, the study area was divided into six sub-regions. Acoustic system and frequency used in the survey were quantitative echo sounder (Simrad Ek 500) and 38, 120-kHz split beam transducers. In order to discriminate krill aggregations in all acoustic signal, difference of mean volume backscattering strength <TEX>$({\Delta}MVBS)$</TEX> method of the two frequencies was introduced. Averaged krill density for the overall surveyed area was <TEX>$23.5g/m^2$</TEX>, and spatially averaged estimates of krill density were <TEX>$44.9g/m^2$</TEX> (north of the South Shetland Islands), <TEX>$30.3g/m^2$</TEX> (Bransfield Strait), <TEX>$11.3g/m^2$</TEX> (near the Elephant Island), <TEX>$13.6g/m^2$</TEX> (north of the Elephant Island), <TEX>$18.1g/m^2$</TEX>(between Elephant Island and South Orkney Islands) and <TEX>$21.7g/m^2$</TEX>(northwest of the South Orkney Islands) at each sub-area. In the two sub-regions with surveyed area, estimated krill biomass in the north of the Elephant Island was 0.315 million tones with a CV of 18.35% <TEX>$(6,766mile^2)$</TEX>, and between Elephant Island and South Orkey Islands was 1.26 million tones with a CV of 9.45% <TEX>$(20,299mile^2)$</TEX>. As a whole, the krill density in the early summer season was low level, comparing with that of January-February. This suggested that major krill swarms in the around South Shetland Islands were reached in the mid-summer seasons from western part of the Antarctic Peninsula, and the low krill density also affects the density variation of the krill between Elephant Island and South Orkney Islands.

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