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Fig. 7.10
Model simulation of the circulation in ice-covered Lake P
ää
j
ä
rvi. Top
—
temperature
cross-section (
Current velocity at 20 m depth.
The maximum depth is 80 m and the length of the lake is 10 km (Huttula et al. 2010)
°
C), Middle
—
Current velocity at 2 m depth, Bottom
—
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