Atmospheric Energetics over the Tropical Pacific during the ENSO Cycle

• Published in: Journal of climate 2017-05, Vol.30 (10), p.3635-3654
• Main Authors: Dong, Di, Li, Jianping, Huyan, Lidou, Xue, Jiaqing
• Format: Article
• Language: English
• Subjects: Anticyclones; Atmospheric sciences; Bursts; Diabatic heating; Earth science; El Nino; El Nino events; El Nino phenomena; El Nino-Southern Oscillation event; Equator; Feedback; Fluid dynamics; Heat transfer; Heating; Kinetic energy; La Nina; La Nina events; Laboratories; Latent heat; Latent heat release; Lower troposphere; Negative feedback; Ocean currents; Ocean temperature; Ocean-atmosphere interaction; Perturbation methods; Physics; Potential energy; Sea surface; Southern Oscillation; Studies; Surface temperature; Tropical climate; Troposphere; Upper troposphere; Wind
• ISSN: 0894-8755; 1520-0442
• DOI: 10.1175/JCLI-D-16-0480.1

The atmospheric perturbation potential energy (PPE) over the tropical Pacific is calculated and analyzed in a composite ENSO cycle. The PPE over the tropical Pacific troposphere increases during El Niño and decreases during La Niña, displaying two centers symmetrical about the equator and delaying the central–eastern Pacific SST anomaly by two months. Generated from atmospheric diabatic heating, the smaller part of PPE in the lower troposphere varies synchronously with the central–eastern Pacific SST through sensible heating, while the larger part of PPE lies in the mid- and upper troposphere and lags the central–eastern Pacific SST about one season because of latent heat release. As the tropical Pacific PPE peaks during the boreal late winter in an El Niño event, two anticyclones form in the upper troposphere as a result of the Gill model response. More PPE is converted to atmospheric kinetic energy (KE) above the central–western Pacific, but less over the eastern Pacific, leading to intensified Hadley circulations over the central–western Pacific and weakened Hadley circulations over the eastern Pacific. The strengthened Hadley circulations cause surface easterly wind bursts through KE convergence in the western equatorial Pacific, which may trigger a La Niña event. The reverse situation occurs during La Niña. Thus, the response of the Hadley circulations in the central–western Pacific provides a negative feedback during the ENSO cycle.