Atmospheric drivers of modelled inaccuracies in heat transport through the Greenland-Scotland ridge. For each CMIP5 model identified by their number as in Table 1, relationship between the 20 year mean poleward heat transport and the 20 year mean atmospheric driver value (left: North Atlantic Oscillation, NAO; centre: East Atlantic pattern, EA; right: Scandinavian pattern, SCA), colour coded by the correlation of their 12-month low-pass filtered time series in a) Denmark Strait (DS); b) Iceland-Faroe ridge (IFR); and c) Faroe-Scotland Channel (FSC). DOI: https://doi.org/10.1525/elementa.354.f7