@ARTICLE{Klusek_Zygmunt_Depth_1988,
author={Klusek, Zygmunt and Godlewska, Małgorzata},
volume={vol. 9},
number={No 2-3},
journal={Polish Polar Research},
pages={349-356},
howpublished={online},
year={1988},
publisher={Polish Academy of Sciences},
publisher={Committee on Polar Research},
abstract={On the basis of hydroacoustic observations it is shown that migrations of krill during spring are stronger than during summer. Migrations of krill are described by the function: H(t) = A + Bcos((2ᴨt/T + φ ) + C c o s ( 2 ᴨt/T + φ ), where: H is depth of the mass center of krill biomass, A — mean depth of krill occurrence, В — amplitude of migrations with period T! = 24 h, С — amplitude of migrations with period T2 = 12 h, (φ1, φ2 — phases of migration process with T, = 24 and T2 = 12 hours. Parameters of the equation are the following: spring — A = 62.2 m, В = 19.5 m, С = 4.6 m, φ1 = 0.1 h, φ2 = 0 . 1 5 h; summer — A = 75.8 m, В = 0.5 m, С = 3.6 m, φ1 = 1.8 h, φ2 = 6.4 h.},
title={Depth distribution and day-night migrations of krill (BIOMASS III, October—November 1986, January 1987)},
type={Article},
URL={http://sd.czasopisma.pan.pl/Content/111281/PDF/1988_2-3_349-356.pdf},
keywords={Antarctica, krill, migrations, BIOMASS III},
}