The Impact of the North Atlantic Oscillation on Climate through Its Influence on the Atlantic Meridional Overturning Circulation

• Published in: Journal of climate Vol. 29; no. 3; pp. 941 - 962
• Main Authors: Delworth, Thomas L., Zeng, Fanrong
• Format: Journal Article
• Language: English
• Published: Boston American Meteorological Society 01.02.2016
• Subjects: Amplitude; Amplitudes; Arctic sea ice; Atlantic Meridional Overturning Circulation (AMOC); Atmosphere; Atmospheric forcing; Brackish; Climate; Climate change; Climate models; Climate system; Deep water; Deep water formation; Density gradients; Heat; Heat flux; Heat transfer; Heat transport; Influence; Marine; Meteorology; Modelling; North Atlantic Oscillation; Ocean-atmosphere system; Oceans; Perturbation; Sea ice; Sea ice temperatures; Simulation; Studies; Temperature; Time; Time series; ANE, North Atlantic, Subpolar Gyre; PN, Arctic; AN, North Atlantic, North Atlantic Oscillation
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/jcli-d-15-0396.1

The impact of the North Atlantic Oscillation (NAO) on the Atlantic meridional overturning circulation (AMOC) and large-scale climate is assessed using simulations with three different climate models. Perturbation experiments are conducted in which a pattern of anomalous heat flux corresponding to the NAO is added to the model ocean. Differences between the perturbation experiments and a control illustrate how the model ocean and climate system respond to the NAO. A positive phase of the NAO strengthens the AMOC by extracting heat from the subpolar gyre, thereby increasing deep-water formation, horizontal density gradients, and the AMOC. The flux forcings have the spatial structure of the observed NAO, but the amplitude of the forcing varies in time with distinct periods varying from 2 to 100 yr. The response of the AMOC to NAO variations is small at short time scales but increases up to the dominant time scale of internal AMOC variability (20–30 yr for the models used). The amplitude of the AMOC response, as well as associated oceanic heat transport, is approximately constant as the time scale of the forcing is increased further. In contrast, the response of other properties, such as hemispheric temperature or Arctic sea ice, continues to increase as the time scale of the forcing becomes progressively longer. The larger response is associated with the time integral of the anomalous oceanic heat transport at longer time scales, combined with an increased impact of radiative feedback processes. It is shown that NAO fluctuations, similar in amplitude to those observed over the last century, can modulate hemispheric temperature by several tenths of a degree.