作者:GUAN Cong,WANG Fan,HU Shijian
摘要:Why did the predicted“super El Niño”fade out in the summer 2014 and the following year develop into one of the three strongest El Niño on record?Although some hypotheses have been proposed in previous studies,the quantitative contribution of oceanic processes to these events remains unclear.We investigated the role of various oceanic feedbacks,especially in response to intra-seasonal westerly wind busts,in the evolution of the 2014–2016 El Niño events,through a detailed heat budget analysis using high temporal resolution Estimating the Circulation and Climate of the Ocean—Phase II(ECCO2)simulation outputs and satellite-based observations.Results show that the Ekman feedback and zonal advective feedback were the two dominant oceanic processes in the developing phase of the warm event in the spring of 2014 and its decay in June.In the 2015–2016 super El Niño event,the zonal advective feedback and thermocline feedback played a signifi cant role in the eastern Pacifi c warming.Moreover,the thermocline feedback tended to weaken in the central Pacifi c where the zonal advection feedback became the dominant positive feedback.
发文机构:Key Laboratory of Ocean Circulation and Waves Center for Ocean Mega-Science Pilot National Laboratory for Marine Science and Technology(Qingdao) College of Marine Science
关键词:ElNiño-SouthernOscillation(ENSO)extremeElNiñozonaladvectivefeedbackthermoclinefeedbackEkmanfeedbackinter-seasonalvariability
分类号: P73[天文地球—海洋科学]