Abstract
Empirical orthogonal function analysis of winter sea surface temperature (SST) anomalies over the Pacific domain (60°N-20°S) reveals an El Nino-Southern Oscillation (ENSO) mode that is linked to the eastern North Pacific, and a North Pacific mode that is linearly independent of ENSO. The North Pacific mode exhibits maximum amplitude and variance explained along ~40°N, west of ~170°W. SSTs in this region have decreased by ~1.5°C from 1950 to 1987. The cooling in winter has been associated with a strengthening of the overlying westerly winds. -Authors
| Original language | English |
|---|---|
| Pages (from-to) | 1677-1680 |
| Number of pages | 4 |
| Journal | Journal of Climate |
| Volume | 8 |
| Issue number | 6 |
| DOIs | |
| State | Published - 1995 |