In order to better understand the global coastal systems and the dangers and risks associated with them, it is important to examine the atmosphere, the land, hydrology, the ocean and especially their interactions
CoastDat-3 (http://www.coastdat.de/about_us/index.php) comprises a compilation of consistent hindcasts obtained from numerical models. The atmospheric part of the dataset is simulated by using the COSMO
coastDat ( https://www.coastdat.de/about_us/index.php.en ) comprises a compilation of coastal analyses obtained from the combination of statistical and numerical models by the Coastal Research institutes
CoastDat-2 (http://www.coastdat.de/about_us/index.php) comprises a compilation of coastal analyses (that is hindcasts and reconstructions) and scenarios for the future obtained from numerical models. The
CoastDat (http://www.coastdat.de/about_us/index.php) comprises a compilaton of coastal analyses (that is hindcasts and reconstructions) and scenarios for the future obtained from numerical models. The
The experiment contains baroclinic hindcast simulations of the North Sea by the hydrodynamic model HAMSOM (Pohlmann, 2006) for the period 1948-2007. HAMSOM was set up at a spatial resolution of 20' x
This is an atmospheric hourly hindcast for Western Europe and the North Atlantic using COSMO-CLM version 4.8_clm_11 with spectral nudging from 1948-2012. The model uses a rotated grid with 254 x 248 grid
The data are from a multi-decadal tide-surge hindcast 1958-2004 for the North Sea using the TELEMAC2D model. Data (sea surface elevation, depth averaged currents) are available every hour on an unstructured
This is an atmospheric hourly hindcast for Western Europe and the North Atlantic using REMO with spectral nudging from 1948-2007. The model uses a rotated grid with 81 x 91 grid points and a grid point
The data are from multi-decadal hindcast simulation with the wave model
WAM 4.5 covering the entire Baltic Sea using a grid size of about 5.5x5.5 km (0.05 degrees latitude x 0.10 degrees longitude). The
This is a North Sea wave hindcast for the period 1949-2014. The simulation has been performed with the wave model WAM Version 4.5.4. The model domain covers the area from 51N to 59N and 4.75W to 13E, with
The data are from multi-decadal hindcast simulation with the wave model WAM 4.5 covering the Southern North Sea (51-56.5 N and -3W-10.5E) using a grid size of about 5,5x5.5 km (0.05 degrees latitude x
This is a hydrodynamic hindcast for the North Sea and the Northeast Atlantic over the period 1948-2015. The simulation has been performed with the hydrodynamic model TRIM-NP V2.1.22 in barotropic 2D mode.
This is a hydrodynamic hindcast for the Baltic Sea over the period 1958-2011. The simulation has been performed with the hydrodynamic model TRIM-NP V2.1 in barotropic 2D mode. Water level and current component
Simulated 2D residual velocity fields in the inner German Bight were
subjected to Principal Component Analysis (PCA). Residual currents
were obtained from coastDat2 barotropic 2D simulations with the