An evaluation of boreal summer intra-seasonal oscillation simulated by BCC_AGCM2.2

• Published in: Climate dynamics Vol. 48; no. 9-10; pp. 3409 - 3423
• Main Authors: Fang, Yongjie, Wu, Peili, Wu, Tongwen, Wang, Zaizhi, Zhang, Li, Liu, Xiangwen, Xin, Xiaoge, Huang, Anning
• Format: Journal Article
• Language: English
• Published: Berlin/Heidelberg Springer Berlin Heidelberg 01.05.2017; Springer; Springer Nature B.V
• Subjects: Analysis; Atmospheric circulation; Atmospheric models; Climate change; Climate models; Climate system; Climatology; Convection; Earth and Environmental Science; Earth Sciences; Environmental aspects; Geophysics/Geodesy; Intergovernmental Panel on Climate Change; Marine; Meteorology; Oceanography; Rain; Summer; Wind; INW, Pacific; China, People's Rep., Beijing; INW, Asia; IN, Pacific; Climate model evaluation; BCC climate model; East Asia summer monsoon; Intra-seasonal oscillation
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-016-3275-4

The intra-seasonal oscillation (ISO) is a prominent feature of the East Asia summer monsoon. The Beijing Climate Center model is one of the IPCC models participating in the Coupled Model Inter-comparison Project (CMIP) 3 and CMIP5 experiments. This paper presents a systematic evaluation of ISO simulated by the Beijing Climate Center atmospheric general circulation model version 2.2 against observations. The model reasonably simulates some salient features of BSISO in terms of temporal spectrum, leading EOF modes, and vertical structure, however limitations are also evident. The strength of the BSISO is overestimated and the northward propagating rain belt is tilted southwest-northeast, which is also different from the observation. The model tends to produce unrealistically strong but shallow convection associated with the ISO, leading to a northward shift of the Western Pacific Subtropical High and the main rain band compared to observations. Process studies show that the anomalous convective heating associated with the wet model bias drives a Gill-type response, resulting in the northwesterly biased position of Western Pacific Subtropical High. The study has revealed how the interaction of moist processes and large-scale dynamics can lead to model bias in simulating the east Asian regional climate system and its variability (ISO in particular). Future improvements in model resolution and convection parameterization are expected to reduce such errors.