In work package 6 of the nextGEMS project, several ocean-only model runs were performed with FESOM (Version 2.0) and ICON-O (Version 2.6.6), to test the sensitivity of the upper tropical Atlantic to different
The concurrent simulation of ocean circulations and ocean tides is carried out with the Max-Planck Institute Ocean Model (MPIOM/TP6M L40 mpiom-1.6.3.) forced by the full luni-solar tidal potential as an
The WOCE/ARGO Global Hydrographic Climatology (WAGHC) is concieved as the update of the previous WOCE Global Hydrographic Climatology (WGHC) (Gouretski and Koltermann, 2004). The following improvements
Reflectances measured in the visible frequency range at three channels of the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard the Earth Observation Satellite (EOS) TERRA were used to derive
Reflectances measured in the visible frequency range at three channels of the Moderate Resolution Imaging Spectroradiometer (MODIS) aboard the Earth Observation Satellite (EOS) TERRA were used to derive
The field campaign LOFZY 2005 (LOFoten ZYklonen, engl.: Cyclones) was carried out in the frame of Collaborative Research Centre 512, which deals with low-pressure systems (cyclones) and the climate system
The drift buoys experiment FRAMZY 2007 consisted of the deployment and tracking of an array of 29 drifting autonomous buoys (16 ice, 13 water) in the Fram Strait region. The buoys were deployed in March
HighRes_highLat_SO FESOM1.4-REcoM2 model simulations to project future change in the coupled physical-biogeochemical system at high Southern Ocean latitudes
This experiment includes all datasets obtained with the global ocean-sea ice-biogeochemistry model FESOM1.4-REcoM2. Model simulations include a representation of ice-shelf cavities and are eddy-permitting
Simulations with the MPI-ESM coupled via energy balance calculation with the ice sheet model PISM. Simulations following four scenarios: a) pre industrial control run (piControl_r1i1p1-P07) b) abrupt
Model output from experiments with the regionally coupled model MPIOM/REMO for the Arctic. External forcing is used ECHAM5 from CMIP3 experiments (for the experiments 437,438,600,601,605,700 and 800).
Model output from experiments with the regionally coupled model MPIOM/REMO for the Arctic. External forcing is used from NCEP/NCAR reanalysis data (for the experiments 436 and 602) and from ECHAM5 from
Data are results of dynamical downscaling of NCEP/NCAR reanalysis, ECHAM5/MPIOM 20th century run and A1B scenario run for the North Atlantic and North European shelves. For the downscaling the global ocean-sea
Simulation with a global high resolution ocean tide and circulation model (MPI-OM with tides), and an embedded thermodynamic sea-ice model, which is explicitly forced by the full lunisolar tidal forcing