Anomalous summer climate in China influenced by the tropical Indo-Pacific Oceans

• Published in: Climate dynamics 2011-02, Vol.36 (3-4), p.769-782
• Main Authors: Weng, Hengyi, Wu, Guoxiong, Liu, Yimin, Behera, Swadhin K, Yamagata, Toshio
• Format: Article
• Language: English
• Subjects: Analysis; Atmosphere. Circulation. Winds; Bgi / Prodig; Climate; Climate change; Climate science; Climatology; Drought; Earth and Environmental Science; Earth Sciences; Earth, ocean, space; El Nino; El Niño; El Niño Modoki; Exact sciences and technology; External geophysics; Flooding; Geophysics/Geodesy; Heat waves; IOD; Marine; Meteorology; Ocean currents; Ocean-atmosphere interaction; Oceanography; Oceans; Physical geography; Rain and rainfall; Regression analysis; Summer climate in China; Summer monsoon; Troposphere; Wind
• ISSN: 0930-7575; 1432-0894
• DOI: 10.1007/s00382-009-0658-9

Possible influences of three coupled ocean-atmosphere phenomena in the Indo-Pacific Oceans, El Niño, El Niño Modoki and the Indian Ocean Dipole (IOD), on summer climate in China are studied based on data analysis for the summers of 1951-2007. Partial correlation/regression analysis is used to find the influence paths through the related anomalous mid- and low-level tropospheric circulations over the oceanic region and East Eurasia, including the western North Pacific summer monsoon (WNPSM). Among the three phenomena, El Niño Modoki has the strongest relationship with the WNPSM. When two or three phenomena coexist with either positive or negative phase, the influences exerted by one phenomenon on summer climate in different regions of China may be enhanced or weakened by other phenomena. In 1994 when both El Niño Modoki and IOD are prominent without El Niño, a strong WNPSM is associated with severe flooding in southern China and severe drought in the Yangtze River Valley (YRV). The 500 hPa high systems over China are responsible for heat waves in most parts of China. In 1983 when a strong negative phase of El Niño Modoki is accompanied by moderate El Niño and IOD, a weak WNPSM is associated with severe flooding in the YRV and severe drought in southern China. The 500 hPa low systems over China are responsible for the cold summer in the YRV and northeastern China. For rainfall, the influence path seems largely through the low-level tropospheric circulations including the WNPSM. For temperature, the influence path seems largely through the mid-level tropospheric circulations over East Eurasia/western North Pacific Ocean.