Meteo-tsunamis are tsunamis that are typically caused by strong atmospheric instability (e.g., pressure jumps) in low pressure systems, but some meteo-tsunamis in winter can be caused by local atmospheric instability in high pressure systems (e.g., the Siberian High). In this study, we investigated a meteo-tsunami event related to a high pressure system that occurred during winter on the Yellow Sea in 2005. Sea level data from tidal stations were analyed with a high-pass filter, and we also performed synoptic weather analyses by using various synoptic weather data (e.g., surface weather charts) collected during the winter season(DJF) of 2005. A numerical weather model (WRF) was used to analyze the atmospheric instability on the day of the selected event (21 Dec. 2005). On the basis of the results, we suggest that the meteo-tsunami triggered by the high pressure system occurred because of dynamic atmospheric instability induced by the expansion and contraction of the Siberian High.

Abstract
 1. 서 론
 2. 연구방법 및 모델개요
  2.1. 연구방법
  2.2. 모델개요
 3. 기상해일 사례일 선정
  3.1. 조위관측자료 분석
  3.2. 종관기상분석
 4. 수치기상모델링
  4.1. 모델 검증
  4.2. 대기구조 분석
 5. 요약 및 토의
 감사의 글
 REFERENCES

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