Articles | Volume 13, issue 17
https://doi.org/10.5194/bg-13-4863-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-13-4863-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Maximum sinking velocities of suspended particulate matter in a coastal transition zone
Institute of Coastal Research, Helmholtz-Zentrum Geesthacht (HZG), Geesthacht, Germany
present address: Max Planck Institute for Meteorology (MPI-M), Hamburg,
Germany
Richard Hofmeister
Institute of Coastal Research, Helmholtz-Zentrum Geesthacht (HZG), Geesthacht, Germany
Eefke M. van der Lee
Institute of Coastal Research, Helmholtz-Zentrum Geesthacht (HZG), Geesthacht, Germany
Ulf Gräwe
Leibniz Institute for Baltic Sea Research, Warnemünde, Germany
Institute of Meteorology and Climatology, Leibniz University Hanover, Hanover, Germany
Rolf Riethmüller
Institute of Coastal Research, Helmholtz-Zentrum Geesthacht (HZG), Geesthacht, Germany
Kai W. Wirtz
Institute of Coastal Research, Helmholtz-Zentrum Geesthacht (HZG), Geesthacht, Germany
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- Estuary-type circulation as a factor sustaining horizontal nutrient gradients in freshwater-influenced coastal systems R. Hofmeister et al. 10.1007/s00367-016-0469-z
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Latest update: 25 Dec 2024
Short summary
We investigated sinking velocity (ws) of suspended particulate matter (SPM) in the German Bight. By inferring ws indirectly from an extensive turbidity data set and hydrodynamic model results, we found enhanced ws in a coastal transition zone. Combined with known residual circulation patterns, this led to a new conceptual understanding of the retention of fine minerals and nutrients in shallow coastal areas. The retention is likely modulated by algal excretions enhancing flocculation of SPM.
We investigated sinking velocity (ws) of suspended particulate matter (SPM) in the German Bight....
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