(from discussion)
...From 1971 to 2000 (Figure 4a) a statistically significant negative correlation between temperature in the Amundsen Sea and SOI can be observed. This suggests that during ENSO warm events (SOI < 0) temperatures in the Amundsen Sea region are warmer, and cooler during ENSO cold events. In contrast the western Ross Sea, including the MDV, is a distinct area where this relationship fails, and no significant correlation can be observed, suggestive of additional or different forces driving temperature variability in this region. Examining the correlations by decade, we find that during 1971–1980 the relationship is similar. During 1981–1990 decade the negative correlation in the Amundsen Sea persists, although its centre shifted further to the northwest. The Ross Sea region and West Antarctica now show a marginal significant positive correlation, indicating cooler temperatures during ENSO warm events. During the 1991–2000 decade, the centre of the Amundsen Sea correlation is shifted southeast, now also encapsulating the adjacent Marie Byrd Land in West Antarctica. The western Ross Sea region displays a highly significant positive correlation, indicating cooler temperatures during ENSO warm events. Together, Figure 4 shows that while the ENSO surface temperature correlation is variable in most regions in Antarctica, the relationship in the Amundsen Sea remains positive and is statistically significant during the last 30 years confirming previous studies [Kwok and Comiso, 2002a, 2002b; Carleton, 2003; Ribera and Mann, 2003; Turner, 2004]. The western Ross Sea, however, exhibits a positive correlation with ENSO at least since 1981. This is consistent with observations of ENSO-correlated increase in sea ice and meridional winds, accompanied by sea surface temperature cooling and lengthening of the sea-ice season in the western Ross Sea and opposing trends in the eastern Ross Sea since 1982 [Kwok and Comiso, 2002b]...(full paper at above link)