NONLINEAR VISUALIZATION OF GEOPHYSICAL DATASETS WITH SELF-ORGANIZING MAPS
SOM-based patterns of sea-ice extent concisely capture the spatial and temporal variability in these data (covering 1973-1996), including the annual progression of expansion and retreat, a general eastward propagation of anomalies during the winter, and subannual variability in the rate of change in extent at different times of the year (e.g., retreat in January is faster than in November). There is also often a general seasonal hysteresis, i.e., monthly anomalies during cooling follow a different spatial path than during warming.
Analysis of North Atlantic MSLP data finds a North Atlantic monopole roughly co-located with the mean position of the Azores High, as well as the well-known North Atlantic Oscillation (NAO) dipole between the subpolar Icelandic Low and the subtropical Azores High. Little trend is shown in December, but the Azores High increased along with the NAO in January and February over the study interval (1957-2002), with implications for storminess in northwestern Europe.
Scientific use of SOMs is increasing rapidly, particularly within the climatology community (including relating ice-core glaciochemistry from Greenland and West Antarctica to atmospheric circulation patterns), yet the power of this technique for data visualization is still to be fully exploited.