caa a22 4500 469100567 CHVBK 20180323133043.0 cr unu---uuuuu 170328e19921101xx s 000 0 eng 10.1007/BF01051363 doi (NATIONALLICENCE)springer-10.1007/BF01051363 Marchenko A. Moscow aut Calculation of wind currents in the edge zone of a sea ice sheet [Elektronische Daten] [A. Marchenko] The steady wind currents in the ocean near the edge of an ice sheet simulated by a rigid cover are studied. The characteristic horizontal scales of the problem correspond to several tens of kilometers. In this case, depending on the depth and viscosity of the fluid, the effect of the Coriolis force on its motion may be comparable with the effect of the wind shear stresses applied to the ice-free surface. Taking the Coriolis force into account leads to the formation of a spiral flow structure in the vertical direction. Plenum Publishing Corporation, 1993 Fluid Dynamics Kluwer Academic Publishers-Plenum Publishers 27/6(1992-11-01), 859-866 0015-4628 27:6<859 1992 27 10697 https://doi.org/10.1007/BF01051363 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1007/BF01051363 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Marchenko A. Moscow aut NATIONALLICENCE 773 0- Fluid Dynamics Kluwer Academic Publishers-Plenum Publishers 27/6(1992-11-01), 859-866 0015-4628 27:6<859 1992 27 10697 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer