54
K. Myrberg and A. Lehmann
Fig. 2.9 Long-term mean surface circulation (cm/s) in the Baltic Sea according to lightship measurements. The persistency of currents is marked as percentages (Palmén 1930; Sjöberg 1992).
From Leppäranta and Myrberg (2009)
2.3.8 Three-Dimensional Water Circulation
The above quasi-permanent cyclonic circulation takes place in the upper layer of
the Baltic Sea. In the lower layer the water dynamics is rather different from that
K. Myrberg and A. Lehmann
Fig. 2.9 Long-term mean surface circulation (cm/s) in the Baltic Sea according to lightship measurements. The persistency of currents is marked as percentages (Palmén 1930; Sjöberg 1992).
From Leppäranta and Myrberg (2009)
2.3.8 Three-Dimensional Water Circulation
The above quasi-permanent cyclonic circulation takes place in the upper layer of
the Baltic Sea. In the lower layer the water dynamics is rather different from that