Summer heat extremes in northern continents linked to developing ENSO events. (6th July 2020)

• Record Type: Journal Article
• Authors: Luo, Ming; Lau, Ngar-Cheung
• Is Part Of: Environmental research letters. Volume 15:Number 7(2020:Jul.)
• Publication Date: 2020-07-06
• Subjects: summer heat extremes -- El Niño-Southern Oscillation -- interannual variability -- circumglobal teleconnection -- jet stream; Environmental sciences -- Periodicals; Human ecology -- Research -- Periodicals; Environmental health -- Periodicals; 333.7
• DOI: 10.1088/1748-9326/ab7d07
• Languages: English
• ISSNs: 1748-9326

Abstract

Abstract: Understanding the variations of extreme weather/climate events is important to improve the seasonal forecast skill of such harmful events. Previous studies have linked boreal summer hot extremes to decaying El Niño-Southern Oscillation (ENSO) events at the interannual scale, but how these hot extreme episodes respond to developing ENSO events remains unclear. Using observational analyses, we demonstrate strong linkages between developing ENSO and extreme heat events in northern continents. In particular, heat extremes in North America, Eastern Europe–Central Asia and Northeast Asia tend to be more frequent during La Niña developing summers and less frequent during El Niño developing phases. Associated atmospheric changes reveal that developing ENSO events feature a circumglobal teleconnection (CGT) pattern over the mid-latitudes. In the La Niña developing summer, this CGT pattern exhibits enhanced geopotential height and anomalous anticyclones over North Pacific, North America, Eastern Europe–Central Asia and Northeastern Asia, and the jet stream generally shifts northward. The atmospheric circulation changes lead to more persistent weather conditions that favor extreme heat events in mid-latitudes. Conversely, opposite changes associated with developing El Niño can inhibit heat extremes in the above locations. The responses of heat extremes to different types (i.e., conventional Eastern Pacific and Modoki Central Pacific) and durations (1 and 2 year) of ENSO events are also discussed.