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Impacts of extreme river discharge on coastal dynamics and environment: Insights from high-resolution modeling in the German Bight

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F24%3A98921" target="_blank" >RIV/60460709:41330/24:98921 - isvavai.cz</a>

  • Result on the web

    <a href="https://doi.org/10.1016/j.rsma.2024.103476" target="_blank" >https://doi.org/10.1016/j.rsma.2024.103476</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.rsma.2024.103476" target="_blank" >10.1016/j.rsma.2024.103476</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Impacts of extreme river discharge on coastal dynamics and environment: Insights from high-resolution modeling in the German Bight

  • Original language description

    The intricate relationship between extreme river discharge and its consequential effects on coastal basins’ environment and dynamics remains a subject of profound significance. The impact of extreme river discharge on coastal basin dynamics and environment is a complex phenomenon, particularly relevant in the context of the German Bight. The inflow of freshwater from rivers into the German Bight plays a crucial role in driving the complex thermohaline circulation. Addressing the challenges posed by local hydro-meteorological extremes, compounded by strong wind waves, currents and tides is vital for comprehensive impact assessment. Utilizing the Geesthacht Coupled cOAstal model SysTem (GCOAST) with high-resolution configuration, we investigate the sensitivity of the thermohaline properties to the river forcings. By incorporating river discharge as lateral land forcing in a coupled hydrodynamic and wave model, we conducted five sensitivity experiments. Our findings reveal that the simulated temperatures closely match measurements in all experiments. The salinity, however, is remarkably sensitive to the variation of freshwater from the rivers Elbe and Ems in the German Bight, causing the haline stratification. The statistical evaluation, as demonstrated by the Taylor diagram at the Marnet DB station, underscores the skill of the Mesoscale Hydrologic Model (mHM) in generating the freshwater discharge that drives the thermohaline characteristics of the German Bight, especially during events like the June 2013 flooding. Significantly, the use of climatological runoff proves to be ineffective in simulating stratification during extreme flooding events. In essence, this investigation enhances our understanding of the pivotal role played by high-frequency river freshwater buoyancy. It emerges as a driving force behind salinity fluctuations during extreme floods, providing valuable insights into coastal dynamics within the German Bight.

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10502 - Oceanography

Result continuities

  • Project

  • Continuities

    S - Specificky vyzkum na vysokych skolach

Others

  • Publication year

    2024

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Regional Studies in Marine Science

  • ISSN

    2352-4855

  • e-ISSN

    2352-4855

  • Volume of the periodical

    2024

  • Issue of the periodical within the volume

    73

  • Country of publishing house

    NL - THE KINGDOM OF THE NETHERLANDS

  • Number of pages

    16

  • Pages from-to

    1-16

  • UT code for WoS article

    001221555700001

  • EID of the result in the Scopus database

    2-s2.0-85189558988