Japan Geoscience Union Meeting 2021

Presentation information

[E] Oral

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

[A-AS02] Extreme Events: Observations and Modeling

Sun. Jun 6, 2021 9:00 AM - 10:30 AM Ch.07 (Zoom Room 07)

convener:Sridhara Nayak(Disaster Prevention Research Institute, Kyoto University), Tetsuya Takemi(Disaster Prevention Research Institute, Kyoto University), Satoshi Iizuka(National Research Institute for Earth Science and Disaster Resilience), Chairperson:Satoshi Iizuka(National Research Institute for Earth Science and Disaster Resilience), Sridhara Nayak(Disaster Prevention Research Institute, Kyoto University), Tetsuya Takemi(Disaster Prevention Research Institute, Kyoto University)

9:45 AM - 10:00 AM

[AAS02-04] Influence of Warm SST in the Oyashio Region on Rainfall Distribution of Typhoon Hagibis (2019)

*Satoshi Iizuka1, Ryuichi Kawamura2, Hisashi Nakamura3, Toru Miyama4 (1.National Research Institute for Earth Science and Disaster Resilience, 2.Department of Earth and Planetary Sciences, Kyushu University, 3.Research Center for Advanced Science and Technology, University of Tokyo, 4.Japan Agency for Marine-Earth Science and Technology,)

Keywords:Typhoon, Rainfall, Sea Surface Temperature, Oyashio

Typhoon Hagibis (2019) caused widespread flooding and damage over eastern Japan. The associated rainfall maxima were primarily observed on the windward mountain slopes along with the west of the leading edge of a low-level front. Concomitantly, a significant positive value in sea surface temperature anomalies (SSTAs) was observed in association with an ocean eddy over the Oyashio region, together with anomalous warmth over the entire western North Pacific. The present study examines the role of the SSTAs in the rainfall distribution associated with Hagibis, to deepen our understanding of the influence of the midlatitude ocean on tropical cyclones and associated rainfall. Our sensitivity experiments demonstrate that the observed warm SSTAs had the potential to displace the rainfall caused by Hagibis inland and thereby acted to increase precipitation along the Pacific coast of northeastern Japan. Our results suggest that midlatitude SSTAs on ocean-eddy scales can also influence the synoptic-scale atmospheric front and associated heavy rainfall.