North Atlantic sea surface temperature data from the Comprehensive Ocean Atmosphere Data Set were used to investigate the behavior of temperature anomalies on multiple-year time scales during the period 1948-1992. Monthly anomaly time series for each two-degree square from the equator to 70 degrees North were low-pass filtered at four years, and normalized by the local standard deviation. Attention is focused on the extreme events, the upper and lower deciles, of the anomaly time series. A 45-year sequence of January maps shows the already familiar phenomena of generally cold conditions prior to 1951, a long warm interval from 1951 through 1967, and again a cold period from 1968 through 1977. The years 1978 through 1982 were largely devoid of persistent strong anomalies, but moderate cold conditions returned during 1983-1986. Warm conditions dominated the North Atlantic from 1987 onward. Within these thermal epochs, however, a total of five cold anomaly features and nine warm anomaly features have been identified. These features have individual lifetimes of three to ten years. A typical size is 20 degrees of latitude or longitude, but they range from barely detectable to spanning the width of the basin, the latter especially in lower latitudes. Most of the anomalies move long distances along certain preferred paths. These paths generally follow the routes of the subarctic and subtropical gyres. Anomalies originating off North America along the boundary between the gyres move northeastward toward the Norwegian Sea along the approximate route of the North Atlantic Current. Midlatitude anomalies originating at the eastern boundary tend to spread both northward and southward along the coast. The speed of these movements (1-3 km per day) is generally less than the expected speed of the near-surface ocean circulation. Simple ideas about the effects of beta dynamics and air-sea heat exchanges were briefly considered, but do not provide a satisfactory explanation for the movements of the anomalies. The long time scale of these extreme events and the continuity of their movements suggests a useful degree of predictability of sea surface temperature based on persistence and propagation of features.
This 6.7 Mbyte QuickTime movie depicts the propagation of anomalies from 1947 to 1992. Step through the first two frames for reference information before starting the movie. In order to view the movie you will need Apple's QuickTime software and player for either the Macintosh or for Windows.