Bild 1 - BALTEX

Conclusions II
• The calculation of ages of inflowing water from
Kattegat or of riverine freshwater in steady-state
requires at least 100-year simulations because
maximum ages are larger than 40 years.
• The downward flux across the halocline caused
by entrainment of the surface water into the
deep water flow can only be balanced by the
upward advective and diffusive fluxes.
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