Database maintenance from 23-Oct-2024 to 30-Oct-2024From 23-Oct-2024 8:00 CEST to 30-Oct-2024 18:00 CEST we will migrate the WDCC database to a new server. During this time metadata input using the metaXA and citeXA applications and DOI registrations will not be available. Data download will still be possible, with the exception of short interruptions, however no new user accounts will be created during the maintenance.
CoastDat-4 (https://www.coastdat.de/about_us/) comprises a compilation of consistent hindcasts obtained from numerical models. The dataset's atmospheric part is simulated using the COSMO in CLimate Mode
CoastDat-3 (https://www.coastdat.de/about_us/) comprises a compilation of consistent hindcasts obtained from numerical models. The atmospheric part of the dataset is simulated by using the COSMO in CLimate
The idea of coastDat (coastdat.de) is to use numerical model-systems to simulate the meteo-marine environment in data sparse regions. For example, the design water level of coastal protection is based,
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
Method description see https://doi.org/10.26050/WDCC/CoastdatStormTides In Version 2 the e (sea_surface_height_above_sea_level variable is corrected for the year 1825. u10 (x_wind), v10 (y_wind) variables correspond to the old version.
The hydrodynamic model Trim-NP (2.6) was used to get an impression of the spatial distribution of water levels at the coast during historical severe storm tides. For these events, the atmospheric reanalysis
This is a wave hindcast for the period 1948 - 2021 covering the North and Baltic Sea. The simulation has been performed with the spectral wave model WAM Version 4.6.2. The model domain covers the area
Regional simulation with the fully coupled physical-biogeochemical model ECOSMO II. Model details and setup specifications are described in Daewel and Schrum (2013). The basis for ECOSMO II is a baroclinic
High RESolution Atmospheric Forcing Fields (HiResAFF) consist of key meteorological variables on daily scale which are typically used to drive ocean or ecosystem models. The fields are reconstructed through
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