Articles | Volume 18, issue 6
https://doi.org/10.5194/os-18-1805-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/os-18-1805-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Imminent reversal of the residual flow through the Marsdiep tidal inlet into the Dutch Wadden Sea based on multiyear ferry-borne acoustic Doppler current profiler (ADCP) observations
Johan van der Molen
CORRESPONDING AUTHOR
Department of Coastal Systems, Royal Netherlands Institute for Sea Research (NIOZ), P.O. Box 59,
1790 AB Den Burg (Texel), the Netherlands
Sjoerd Groeskamp
Department of Coastal Systems, Royal Netherlands Institute for Sea Research (NIOZ), P.O. Box 59,
1790 AB Den Burg (Texel), the Netherlands
Leo R. M. Maas
Institute for Marine and Atmospheric Research (IMAU), Utrecht
University, Princetonplein 5, 3584 CC Utrecht, the Netherlands
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Short summary
We studied the long-term mean flow through the Marsdiep tidal inlet in the Dutch Wadden Sea. We found that this flow, which is important for sediment, salt and nutrient balances, is reversing from net outflow to inflow. We hypothesise changes in tides in the North Sea caused this, due to increased stratification in response to global warming. Hence, we expect permanent inflow conditions within 1 decade, with potential effects on the sediment balance and the ecosystem of this World Heritage Site.
We studied the long-term mean flow through the Marsdiep tidal inlet in the Dutch Wadden Sea. We...