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Documentation below is provided as is. The dataset the documentation below relates to is no longer supported and will be removed from the Climate Data Store (CDS) at a later date. |
Contributors: A. Hall (TVUK), J. Marsh (TVUK), J. Clark (Plymouth Marine Laboratory), S. Kay (Plymouth Marine Laboratory), J. A. Fernandes (AZTI)
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Introduction...
- The Northeast Atlantic domain (NEMO model)
- CMIP5 driving model: Met Office Hadley Centre (MOHC) Hadley Global Environment Model 2 – Earth System (HadGEM2-ES). Further information regarding the model is available here: https://portal.enes.org/models/earthsystem-models/metoffice-+%20hadley-centre/hadgem2-es
- Regional climate model: SMHI RCA4, as for the pan-European domain
- Greenhouse gas concentration scenarios: RCP 4.5 and RCP 8.5
- Variables: 6 hourly surface forcing 10 m wind components, sea level pressure, 2 m air temperature and relative humidity, daily precipitation, shortwave and longwave radiation flux and cloud cover
- The pan-European domain (POLCOMS model)
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The datasets are provided through the Copernicus Climate Change Service (C3S) Climate Data Store (CDS):
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Quality Assurance...
There is also a good spatial and temporal match between modelled and satellite-derived sea surface temperature. The reanalysis-driven run of the model tends to overestimate sea surface temperature in shelf waters, especially in the spring and summer. The GCM-driven run has higher bias, and over-estimates winter temperatures in much of the region. This is in line with the biases in the HadGEM2-ES model driving the model. Model-satellite correlation is high in all regions, though rather lower for the GCM-driven run: as noted above, a climate model is not expected to accurately reproduce conditions month-by-month, even in a hindcast.
Copernicus Climate Change Service
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