Two Types of El Niño Events Cold Tongue El Niño and Warm Pool El Niño

• Published in: Journal of climate Vol. 22; no. 6; pp. 1499 - 1515
• Main Authors: Kug, Jong-Seong, Jin, Fei-Fei, An, Soon-Il
• Format: Journal Article
• Language: English
• Published: Boston, MA American Meteorological Society 15-03-2009
• Subjects: Advection; Anomalies; Atmospherics; Climate; Climate models; Cold; Data analysis; Data assimilation; Earth, ocean, space; El Nino; El Nino events; El Nino phenomena; Enthalpy; Exact sciences and technology; External geophysics; Feedback; Global climate models; Heat content; Marine; Meteorology; Noise; Ocean currents; Ocean temperature; Oceanic analysis; Oceans; Physics of the oceans; Precipitation; Sea level; Sea surface; Sea surface temperature; Sea surface temperature anomalies; Sea-air exchange processes; Southern Oscillation; Surface temperature; Thermocline; Equatorial Pacific; Pacific Ocean; Process dynamics; Temperature distribution; Spatial distribution; El Nino; Transition; Observation data; Sea surface temperature; ocean-atmosphere interaction; anomalies; Formation mechanism; Composite analysis; Data assimilation
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/2008jcli2624.1

In this study, two types of El Niño events are classified based on spatial patterns of the sea surface temperature (SST) anomaly. One is the cold tongue (CT) El Niño, which can be regarded as the conventional El Niño, and the other the warm pool (WP) El Niño. The CT El Niño is characterized by relatively large SST anomalies in the Niño-3 region (5°S–5°N, 150°–90°W), while the WP El Niño is associated with SST anomalies mostly confined to the Niño-4 region (5°S–5°N, 160°E–150°W). In addition, spatial patterns of many atmospheric and oceanic variables are also distinctively different for the two types of El Niño events. Furthermore, the difference in the transition mechanism between the two types of El Niño is clearly identified. That is, the discharge process of the equatorial heat content associated with the WP El Niño is not efficient owing to the spatial structure of SST anomaly; as a result, it cannot trigger a cold event. It is also demonstrated that zonal advective feedback (i.e., zonal advection of mean SST by anomalous zonal currents) plays a crucial role in the development of a decaying SST anomaly associated with the WP El Niño, while thermocline feedback is a key process during the CT El Niño.