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
The concentrations and deposition of atmospheric constituents such as air pollutants were modeled with the Community Multiscale Air Quality (CMAQ) Model system for the year 2008. A focus was on sea salt
COSMO-CLM simulation for Bohai, Yellow and East China Sea:
System Analysis and Modelling Group at the Helmholtz-Zentrum Geesthacht Centre for Materials and Coastal Research (referred to hereinafter as
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
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
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
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 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
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
Simulations were performed over two time periods in winter and summer 2008 (a third period in the base case). Each period was preceded by a 10 day spin-up phase started from a standard initial condition
Simulations were performed over two time periods in winter and summer 2008 (a third period in the base case). Each period was preceded by a 10 day spin-up phase started from a standard initial condition
Simulations were performed over two time periods in winter and summer 2008 (a third period in the base case). Each period was preceded by a 10 day spin-up phase started from a standard initial condition
Simulations were performed over two time periods in winter and summer 2008 (a third period in the base case). Each period was preceded by a 10 day spin-up phase started from a standard initial condition
Simulations were performed over two time periods in winter and summer 2008 (a third period in the base case). Each period was preceded by a 10 day spin-up phase started from a standard initial condition