Rainfall is an essential meteorological parameter describing the monsoon climate. Rainfall distribution indicates the location of the atmospheric heat source that drives tropical circulation; thus, rainfall variation reflects the variability of the entire monsoon circulation system. Rainfall is also a key component of the hydrological cycle of the earth's climate system, playing a central role in connecting terrestrial, atmospheric, and oceanic processes. The study of rainfall characteristics is of central importance for understanding monsoon circulation and its relationship with other components of the hydrological cycle. The majority of the literature dealing with Asian monsoon rainfall climatology has been devoted to depicting rainy seasons over the land and islands using rain gauge observations e.
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The Asian Games , also known as Asiad ,  is a continental multi-sport event held every four years among athletes from all over Asia. There have been nine nations that have hosted the Asian Games. Forty-six nations have participated in the Games, including Israel , which was excluded from the Games after their last participation in The most recent games was held in Jakarta and Palembang , Indonesia from 18 August to 2 September
For more than fifteen years, the Department of East Asian Languages and Literatures has offered intensive language training in Japanese during summer months. These summer courses challenge your resolve but reward you with rapid language acquisition with a strong proficiency in aural comprehension and oral communication in addition to basic reading and writing skills. Click here to view the flyer for Summer These two classes have a special ten-week span: it starts two weeks later than Pitt's regular week summer term.
The Indian and East Asian summer monsoons are two components of the whole Asian summer monsoon system. Previous studies have indicated in-phase and out-of-phase variations between Indian and East Asian summer rainfall. The present study reviews the current understanding of the connection between Indian and East Asian summer rainfall. The review covers the relationship of northern China, southern Japan, and South Korean summer rainfall with Indian summer rainfall; the atmospheric circulation anomalies connecting Indian and East Asian summer rainfall variations; the long-term change in the connection between Indian and northern China rainfall and the plausible reasons for the change; and the influence of ENSO on the relationship between Indian and East Asian summer rainfall and its change.