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Observations from the global array of tide gauges show that global sea-level has been rising at an average rate of 1.5-2 mm/yr during the last ~150 years [Douglas 1991, Spada and Galassi 2012]. Althou...
During the last glacial maximum, a large ice sheet covered Scandinavia, which depressed the earth's surface by several 100 m. In northern central Europe, mass redistribution in the upper mantle led to...
Computation of the Evaporation from the Baltic Sea from the Flux of Water Vapor in the Atmosphere
Using monthly mean sea level data from Stockholm since 1825, the longest unbroken series of such data in the world, we have analysed the secular increase of the seasonal sea level variation in the Ba...
The freshwater input in to estuarine areas sets the scene for the stratification and the current field of the uppermost layer of the seas. Different dynamical features are relatively simple to disting...
Sea ice drift in the coastal ice zone of the Bothnian Bay was measured with five GPS drifters in March 1997. To model coastal ice dynamics, the viscous-plastic ice model of Hibler with a fine spatial ...
Marine meteorological conditions and air-sea exchange processes over the northern Baltic Sea were studied using data from three open-sea lighthouse meteorological stations and the R/V Aranda automati...
Superimposed ice formation and sub-surface melting were modelled using a one-dimensional thermodynamic sea ice model with the Baltic Air-Sea-Ice Study (BASIS) field data. During a thermal equilibrium...
The living benthic foraminiferal assemblages in Kiel Fjord (SW Baltic Sea) were investigated in the years 2005 and 2006. The faunal studies were accomplished by geochemical analyses of surface sedimen...

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