Forced and Internal Twentieth-Century SST Trends in the North Atlantic

Publication Type  Journal Article
Year of Publication  2009
Authors  Ting, M. F.; Kushnir, Y.; Seager, R.; Li, C. H.
Journal Title  Journal of Climate
Volume  22
Issue  6
Pages  1469-1481
Journal Date  Mar
ISBN Number  0894-8755
Accession Number  ISI:000265104000010
Key Words  sea-surface temperature; hurricane activity; climate; rainfall; variability; circulation; oscillation; summer; model
Abstract  

In recent years, two alarming trends in North Atlantic climate have been noted: an increase in the intensity and frequency of Atlantic hurricanes and a rapid decrease in Greenland ice sheet volume. Both of these phenomena occurred while a significant warming took place in North Atlantic sea surface temperatures (SSTs), thus sparking a debate on whether the warming is a consequence of natural climate variations, anthropogenic forcing, or both; and if both, what their relative roles are. Here models and observations are used to detect and attribute long-term (multidecadal) twentieth-century North Atlantic (NA) SST changes to their anthropogenic and natural causes. A suite of Intergovernmental Panel on Climate Change (IPCC) twentieth-century (C20C) coupled model simulations with multiple ensemble members and a signal-to-noise maximizing empirical orthogonal function analysis are used to identify a model-based estimate of the forced, anthropogenic component in NA SST variability. Comparing the results to observations, it is argued that the long-term, observed, North Atlantic basin-averaged SSTs combine a forced global warming trend with a distinct, local multidecadal "oscillation" that is outside of the range of the model-simulated, forced component and most likely arose from internal variability. This internal variability produced a cold interval between 1900 and 1930, followed by 30 yr of relative warmth and another cold phase from 1960 to 1990, and a warming since then. This natural variation, referred to previously as the Atlantic Multidecadal Oscillation (AMO), thus played a significant role in the twentieth-century NA SST variability and should be considered in future, near-term climate projections as a mechanism that, depending on its behavior, can act either constructively or destructively with the region's response to anthropogenic influence, temporarily amplifying or mitigating regional climate change.

Notes  

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URL  <Go to ISI>://000265104000010
DOI  Doi 10.1175/2008jcli2561.1