Impact of Surface Sensible Heating over the Tibetan Plateau on the Western Pacific Subtropical High： A Land-Air-Sea Interaction Perspective

• Published in: Advances in atmospheric sciences Vol. 34; no. 2; pp. 157 - 168
• Main Authors: Duan, Anmin, Sun, Ruizao, He, Jinhai
• Format: Journal Article
• Language: English
• Published: Heidelberg Science Press 01.02.2017; Springer Nature B.V; University of Chinese Academy of Sciences, Beijing 100049, China%Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters,Nanjing University of Information Science and Technology, Nanjing 210044, China; State Key Laboratory of Numerical Modelling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
• Subjects: Atmospheric circulation; Atmospheric Sciences; Cyclones; Earth and Environmental Science; Earth Sciences; El Nino; Geophysics/Geodesy; Marine; Meteorology; Ocean currents; Ocean-atmosphere interaction; Original Paper; Spring; Summer; China, People's Rep., Xizang, Tibetan Plateau; INW, Pacific; I, Central Pacific; IW, Pacific; tropical air–sea interaction; surface sensible heating; Tibetan Plateau; western Pacific subtropical high; ENSO; tropical air-sea interaction
• ISSN: 0256-1530; 1861-9533
• DOI: 10.1007/s00376-016-6008-z

The impact of surface sensible heating over the Tibetan Plateau （SHTP） on the western Pacific subtropical high （WPSH） with and without air-sea interaction was investigated in this study. Data analysis indicated that SHTP acts as a relatively independent factor in modulating the WPSH anomaly compared with ENSO events. Stronger spring SHTP is usually fol- lowed by an enhanced and westward extension of the WPSH in summer, and vice versa. Numerical experiments using both an AGCM and a CGCM confirmed that SHTP influences the large-scale circulation anomaly over the Pacific, which features a barotropic anticyclonic response over the northwestern Pacific and a cyclonic response to the south. Owing to different background circulation in spring and summer, such a response facilitates a subdued WPSH in spring but an en- hanced WPSH in summer. Moreover, the CGCM results showed that the equatorial low-level westerly at the south edge of the cyclonic anomaly brings about a warm SST anomaly （SSTA） in the equatorial central Pacific via surface warm advection. Subsequently, an atmospheric Rossby wave is stimulated to the northwest of the warm SSTA, which in turn enhances the at- mospheric dipole anomalies over the western Pacific. Therefore, the air-sea feedbacks involved tend to reinforce the effect of SHTP on the WPSH anomaly, and the role of SHTP on general circulation needs to be considered in a land-air-sea interaction framework.