Japan Geoscience Union Meeting 2022

Presentation information

[E] Oral

A (Atmospheric and Hydrospheric Sciences ) » A-AS Atmospheric Sciences, Meteorology & Atmospheric Environment

[A-AS08] Multiple scale structure and their interactions in Asian monsoon system

Mon. May 23, 2022 3:30 PM - 5:00 PM 101 (International Conference Hall, Makuhari Messe)

convener:Toru Terao(Faculty of Education, Kagawa University), convener:Shinjiro Kanae(School of Environment and Society, Tokyo Institute of Technology), Jun Matsumoto(Deaprtment of Geography, Tokyo Metropolitan University), Chairperson:Masafumi Hirose(Meijo University)

3:45 PM - 4:00 PM

[AAS08-08] Early Indian Summer Monsoon Onset Driven by Low Soil Moisture in the Iranian region

*Suyeon Moon1,2, Kyung-Ja Ha1,2,3 (1.Department of Climate System, Pusan National University, Busan, South Korea, 2.Center for Climate Physics, Institute for Basic Science, Busan, South Korea, 3.BK21 School of Earth and Environmental Systems, Pusan National University, Busan, South Korea)

Keywords:soil moisture, summer monsoon onset, precursor of monsoon onset, Indian summer monsoon

Advancing the leading time for onset prediction of the Indian summer monsoon (ISM) onset is an imperative task. However, it has remained a challenging subject. In particular, the land-atmosphere coupling associated with monsoon onset prediction is poorly understood. Here we attempt to investigate the land factor as the ISM onset precursor by studying the internal mechanism of atmospheric heating, which is distinguished by monsoon onset. The low (high) soil moisture in the Iranian region during March and April advances (delays) ISM onset by enhancing (disturbing) the vertical easterly wind shear. In addition, mid-tropospheric heating is affected by soil moisture in the Iranian region. By investigating the internal atmospheric heating process and suggesting the relationship between low soil moisture and ISM onset, these findings clarify the monsoon onset mechanism in terms of the vertical atmospheric profile and land-atmosphere interaction, which eventually extend the lead time for the onset prediction.