The Atlantic inflow across the Greenland-Scotland ridge in global climate models (CMIP5)
Oceanic heat transport from the North Atlantic to the Arctic through the Nordic Seas is a key component of the climate system that has to be modelled accurately in order to predict, for example, future Arctic sea ice changes or European climate. Here we quantify biases in the climatological state an...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
BioOne
2019-05-01
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| Series: | Elementa: Science of the Anthropocene |
| Subjects: | |
| Online Access: | https://www.elementascience.org/articles/354 |