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Felix W. Landerer, Johann H. Jungclaus, and Jochem Marotzke

simulated halosteric expansion and contraction? Regional salinity changes are a consequence of changes in the local freshwater balance, for example, induced by changes in the hydrological cycle (precipitation, evaporation, and river runoff: P − E + R ), anomalous salt advection in the ocean, or altered sea ice volume. Increased atmospheric moisture transport from lower to high latitudes is a common feature of many climate scenario simulations ( Bryan 1996 ; Mikolajewicz and Voss 2000 ; Thorpe et al

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