Abstract

The seasonality of the ENSO-rainfall relationship in central Chile (30°-41°S) and associated circulation anomalies are studied using correlation and compositing techniques. During El Niño episodes there is a tendency for the occurrence of above-average precipitation between 30° and 35°S in winter [June-July-August (JJA)] and from 35° to 38°S in late spring [October November (ON)]. while rainfall deficit is typically observed from around 38° to 41°S during the following summer [January-February-March (JFM)], when El Niño reaches its maximum development. Opposite rainfall anomalies are characteristic during La Niña events. This study confirms results from previous investigations indicating that enhanced blocking activity over the Amundsen-Bellingshausen Seas area in the southeastern (SE) Pacific during El Niño is a key feature explaining the wet conditions in winter. It is also shown that the same circulation anomaly explains the relatively wet conditions in late spring in the 35°-38°S region during El Niño episodes. Furthermore, the southward displacement from winter to late spring of the area with significant ENSO-related rainfall anomalies seems associated with the seasonal migration of the boundary separating the region under the influence of the subtropical domain from the extratropical domain, where the westerly regime and associated disturbances prevail. Blocking episodes in the SE Pacific during El Niño seem to be part of a wave structure, particularly intense during spring, characterized by a sequence of positive and negative quasi-barotropic height anomalies stretching southeastward from the equator toward the SE Pacific and back to the southwestern Atlantic. On the other hand, anomalously dry conditions in winter and late spring during La Niña are favored by long-lasting and intense ridges at subtropical latitudes over the SE Pacific and South America resulting in a southward migration of the midlatitude storm tracks. In summer, a higher frequency of ridges in the southern tip of the South America during El Niño episodes presumably contributes to reinforcement of the southern edge of the subtropical anticyclone in the SE Pacific, which at this time of the year reaches its southernmost position, resulting in the annual rainfall minimum. On the other hand, an increased frequency of cyclonic circulation anomalies crossing the southern tip of the continent is associated with relatively wet conditions in southern-central Chile, particularly during La Niña events.