Thermal Controls on the Asian Summer Monsoon

• Published in: Scientific reports 2012-05, Vol.2 (1), p.404, Article 404
• Main Authors: Wu, Guoxiong, Liu, Yimin, He, Bian, Bao, Qing, Duan, Anmin, Jin, Fei-Fei
• Format: Article
• Language: English
• Subjects: 704/106/242; 704/106/35; 704/106/694; 704/172; Asia; Climate; Climate change; Ecosystem; ENVIRONMENTAL SCIENCES; Geography; Global climate; Human influences; Humanities and Social Sciences; Humans; Models, Theoretical; Monsoons; multidisciplinary; Ocean currents; Oceans and Seas; Rain; Science; Science & Technology - Other Topics; Seasons; Temperature; Water Movements; Wind
• ISSN: 2045-2322; 2045-2322
• DOI: 10.1038/srep00404

The Asian summer monsoon affects more than sixty percent of the world's population; understanding its controlling factors is becoming increasingly important due to the expanding human influence on the environment and climate and the need to adapt to global climate change. Various mechanisms have been suggested; however, an overarching paradigm delineating the dominant factors for its generation and strength remains debated. Here we use observation data and numerical experiments to demonstrates that the Asian summer monsoon systems are controlled mainly by thermal forcing whereas large-scale orographically mechanical forcing is not essential: the South Asian monsoon south of 20°N by land–sea thermal contrast, its northern part by the thermal forcing of the Iranian Plateau and the East Asian monsoon and the eastern part of the South Asian monsoon by the thermal forcing of the Tibetan Plateau.