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    AMSeLOstsee : Analyse von hochauflösenden Wasserstandsverläufen und Ermittlung des MSL sowie von Extremwasserständen an der südlichen und südwestlichen Ostseeküste
    (Bundesanstalt für Wasserbau, 2022) ; ; ; ;
    The collaborative project AMSeLBaltic Sea (03KIS0114 & 03KIS0115) was carried out between 2015 and 2018 by the Research Institute for Water and Environment (fwu) at the University of Siegen and the Institute of Hydraulic Engineering at the Technical University Hamburg-Harburg. In particular, the investigation concentrated on the research, acquisition, processing and, if necessary, additional digitisation of available sea level data in the Baltic Sea with a focus on the southern and south-western Baltic Sea coast. On the basis of the total available sea level time series with different temporal resolutions, long-term and high-quality monthly time series of the mean sea level (MSL) as well as extreme sea level time series were generated and investigated.
    Publicationtype: Journal Article
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      66
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    Geocentric mean sea level fields at the German North Sea and Baltic coast
    Global mean sea level has risen over the 20th century (Hay et al. 2015; Dangendorf et al. 2017) and under sustained greenhouse gas emissions it is projected to further accelerate throughout the 21st century (Church et al. 2013) with large spatial variations, significantly threatening coastal communities. Locally the effects of geocentric (sometimes also referred to absolute) sea level rise can further be amplified by vertical land motion (VLM) due to natural adjustments of the solid earth to the melting of the large ice-sheets during the last deglaciation (GIA) or local anthropogenic interventions such as groundwater or gas withdrawal (e.g. Santamaría-Gómez et al. 2017). Both, the observed and projected geocentric sea level rise as well as VLM are critically important for coastal planning and engineering, since only their combined effect determines the total threat of coastal flooding at specific locations. Furthermore, due large spatial variability of sea level, information is required not only at isolated tide gauge (TG) locations but also along the coastline stretches in between.
    Publicationtype: Conference Paper
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