A meteo-tsunami occurred along the coastline of South Korea on 31 March 2007, with an estimated maximum amplitude of 240 cm in Yeonggwang (YG). In this study, we investigated the synoptic weather systems around the Yellow sea including the Bohai Bay and Shandong Peninsula using a weather research and forecast model and weather charts of the surface pressure level, upper pressure level and auxiliary analysis. We found that 4-lows passed through the Yellow sea from the Shandung Peninsula to Korea during 5 days. Moreover, the passage of the cold front and the locally heavy rain with a sudden pressure change may make the resonance response in the near-shore and ocean with a regular time-lag. The sea-level pressure disturbance and absolute vorticity in 500 hPa projected over the Yellow sea was propagated with a similar velocity to the coastline of South Korea at the time that meteo-tsunami occurred.

Abstract
 1. 서 론
 2. 연구방법
  2.1. 해수면 관측자료 분석
  2.2. 종관기상분석
  2.3. 기상모델
 3. 기상해일 및 일기도 분석
  3.1. 기상해일 도달시각 분석
  3.2. 지상일기도 분석
  3.3. 대기 연직구조 분석
 4. 기상모델링 결과 분석
 5. 결 론
 감사의 글
 참고문헌

• 김현수(부산대학교 지구환경시스템학부) | Hyunsu Kim (Department of Atmospheric Science, Pusan National University)
• 김유근(부산대학교 지구환경시스템학부) | Yoo-Keun Kim (Department of Atmospheric Science, Pusan National University) Corresponding author
• 우승범(인하대학교 해양과학과) | Seung-Buhm Woo (Department of Oceanography, Inha University)
• 김명석(인하대학교 해양과학과) | Myung-Seok Kim (Department of Oceanography, Inha University)