Articles | Volume 12, issue 4
Ocean Sci., 12, 977–986, 2016
https://doi.org/10.5194/os-12-977-2016
Ocean Sci., 12, 977–986, 2016
https://doi.org/10.5194/os-12-977-2016

Research article 18 Aug 2016

Research article | 18 Aug 2016

Effects of surface current–wind interaction in an eddy-rich general ocean circulation simulation of the Baltic Sea

Heiner Dietze and Ulrike Löptien

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Cited articles

Carstensen, J., Andersen, J. H., Gustafsson, B. G., and Conley, D. J.: Deoxygenation of the Baltic Sea during the last century, PNAS, 111, 5628–5633, 2014.
Dewar, W. K. and Flierl, G. R.: Some Effects of the Wind on Rings, J. Phys. Oceanogr., 17, 1653–1667, 1987.
Dietze, H. and Kriest, I.: 137Cs off Fukushima Dai-ichi, Japan – model based estimates of dilution and fate, Ocean Sci., 8, 319–332, https://doi.org/10.5194/os-8-319-2012, 2012.
Dietze, H. and Löptien, U.: Revisiting “nutrient trapping” in global coupled biogeochemical ocean circulation models, Global Biogeochem. Cy., 27, 265–284, 2013.
Dietze, H. and Oschlies, A.: Modeling abiotic production of apparent oxygen utilisation in the oligotrophic subtropical North Atlantic, Ocean Dynam., 55, 28–33, 2005.
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Short summary
Winds blowing over the ocean drive ocean currents. The oceanic response to winds is, in turn, influenced by ocean currents. Theoretical considerations suggest that the latter effect is especially pronounced in the Baltic Sea. The study presented here puts theses theoretical considerations in a high-resolution ocean circulation model of the Baltic Sea to the test.