日本地球惑星科学連合2025年大会

講演情報

[E] ポスター発表

セッション記号 A (大気水圏科学) » A-AS 大気科学・気象学・大気環境

[A-AS03] Extreme Events and Mesoscale Weather: Observations and Modeling

2025年5月27日(火) 17:15 〜 19:15 ポスター会場 (幕張メッセ国際展示場 7・8ホール)

コンビーナ:竹見 哲也(京都大学防災研究所)、Nayak Sridhara(Japan Meteorological Corporation)、下瀬 健一(国立研究開発法人防災科学技術研究所)、本田 匠(東京大学情報基盤センター)

17:15 〜 19:15

[AAS03-P09] Definition of a new East Asian subtropical summer monsoon index

*hongming yan1 (1.Yunnan Meteorological Administration)

キーワード:East Asian summer monsoon, Summer rainfall in China, Three kinds of rainfall pattern, Circulation anomalies over northwestern Pacific

Based on precipitation data of 160 observation stations in China and NCEP / NCAR reanalysis atmospheric circulation data from 1958 to 2014, the relationship between summer precipitation in China and wind at low and high level is firstly investigated. Then a new East Asian subtropical summer monsoon index is defined using 200-hPa zonal wind closely relating to three kinds of summer rainfall in Eastern China. The results show that the new index may well reflect not only the integrated impact of the circulations over high and low latitudes, but also summer precipitation difference characteristic between northern and southern China. Strong East Asian summer monsoon years, strengthen high-level westerly, North position of cold air activity, strengthen the low-level West Pacific subtropical high pressure with position to the north resulting in strong south-west flow over Eastern East Asian, type I rainfall occurring to Eastern China; circulation changes is just the opposite in weak East Asian summer monsoon, type Ⅲ rainfall occurring to Eastern China. Compared with the existing East Asian summer monsoon index, the new index has a great advantage in reflecting the precipitation difference between eastern and southern China.