2026-05-28T18:05:06Z http://dmoai.cloud.dkrz.de/oai/provider

oai:wdcc.dkrz.de:iso_3880338 2026-05-27T23:08:45Z iso-wdcc-doi

wdc-climate.de:3880338 eng; USA collection ECC-BRS_HAMSOM Mihael Machado de Souza University of Hamburg https://www.ifm.uni-hamburg.de/en.html pointOfContact Mihael Machado de Souza University of Hamburg https://www.ifm.uni-hamburg.de/en.html pointOfContact 2020-08-04T14:42:38 ISO 19115 ISO 19115-2:2009 Model output prepared in support of the analysis of impacts to the stratification along the Brazilian shelf under a strong warming scenario (RCP8.5) 2020-08-14 publication 1 ECC-BRS_HAMSOM doi:10.26050/WDCC/ECC-BRS_HAMSOM Mihael Machado de Souza University of Hamburg https://www.ifm.uni-hamburg.de/en.html Email: mihael.de.souza@uni-hamburg.de principalInvestigator Mihael Machado de Souza University of Hamburg https://www.ifm.uni-hamburg.de/en.html Email: mihael.de.souza@uni-hamburg.de author Dr. Moritz Mathis Helmholtz-Zentrum Geesthacht, Zentrum für Material- und Küstenforschung GmbH not filled Email: moritz.mathis@hereon.de author Dr. Thomas Pohlmann University of Hamburg https://www.ifm.uni-hamburg.de/en.html Email: thomas.pohlmann@uni-hamburg.de author WDC Climate at DKRZ publisher This experiment aims to investigate the impact of anthropogenic climate change to the stratification of the Brazilian shelf waters under a strong warming scenario (RCP8.5). Earth System Models (ESMs) predict a stronger increase in stratification over the equatorial regions, due to the increased surface warming. However, they cannot account for all relevant regional processes due to their coarse horizontal resolution. One of the more relevant local processes unresolved by ESMs is the upwelling of South Atlantic Central Water along subtropical Brazil. It brings cold and nutrient-rich waters towards the coast to the most productive shelf regions along the Brazilian coastal waters and is known to play an important role in the stratification of the South Brazil Bight. By including this process in our analysis through our downscaling experiment, we can provide a more complete assessment of the effects of increased greenhouse gas emissions in the stratification of the Brazilian continental shelf. Mihael Machado de Souza University of Hamburg https://www.ifm.uni-hamburg.de/en.html pointOfContact NetCDF CC-BY-4.0: Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ eng; USA -54.9672 -33.0515 -36.9481 -1.7829 proleptic_gregorian 1970-01-16 2100-12-16 sea_surface_temperature Sea surface temperature is usually abbreviated as "SST". It is the temperature of sea water near the surface (including the part under sea-ice, if any), and not the skin temperature, whose standard name is surface_temperature. For the temperature of sea water at a particular depth or layer, a data variable of sea_water_temperature with a vertical coordinate axis should be used. [CF-Standard Name]; unit: not filled potential_energy_anomaly_due_to_salinity not filled; unit: not filled maximum_density_gradient not filled; unit: not filled depth_of_max_density_gradient not filled; unit: not filled potential_energy_anomaly_due_to_temperature not filled; unit: not filled potential_energy_anomaly not filled; unit: not filled sea_surface_salinity The unit of salinity is PSU, which is dimensionless. The units attribute should be given as 1e-3 or 0.001 i.e. parts per thousand if salinity is in PSU. Sea surface salinity is often abbreviated as "SSS". For the salinity of sea water at a particular depth or layer, a data variable of sea_water_salinity with a vertical coordinate axis should be used. [CF-Standard Name]; unit: not filled NetCDF 29493 https://www.wdc-climate.de/ui/entry?acronym=ECC-BRS_HAMSOM information collection n/a None n/a None