In models, AMO-like variability is associated with small changes in the North Atlantic branch of the Thermohaline Circulation, however historical oceanic observations are not sufficient to associate the derived AMO index to present day circulation anomalies.
AMO-like variability is associated with small changes in the North Atlantic branch of the Thermohaline Circulation. This was in models. Historical oceanic observations are not sufficient to associate the derived AMO index to present day circulation anomalies. This is in models.