This work investigates the relationship between the sea breeze circulation and ozone concentrations during cold water events in the southeastern coastal area of the Korean Peninsula, where coastal upwelling frequently occur.
This analysis was performed based on the classification of two categories, such as cold water and non-cold water events, over the period of 2000-2009. The low air temperature (0.5℃), low SST (5℃) and the wind direction(southerly) are the features of the cold water events in the Southeastern coastal area. Moreover, ozone concentrations in the cases of the sea breeze circulation and cold water events were significantly lower (below 30 ppb) than those (70∼100 ppb) in the non-clod water events, because of the low air temperature (10∼20℃) and high wind speed (3∼5 m/s) around the southeastern coastal area.

Abstract
 1. 서 론
 2. 연구 및 방법
  2.1. 대상지역
  2.2. 연구방법
 3. 결과
  3.1 냉수대의 발달과 기상변화
  3.2. 냉수대 발생과 중규모 순환의 영향
 4. 결 론
 참 고 문 헌

• 지효은(부산대학교 환경연구원) | Hyo Eun Ji (Institute of Environmental Studies, Pusan National University)
• 박창현(부산대학교 환경연구원) | Changhyoun Park (Institute of Environmental Studies, Pusan National University)
• 이순환(부산대학교 지구과학 교육학과) | Soon-Hwan Lee (Department of Earth Science Education, Pusan National University)
• 이화운(부산대학교 지구환경시스템 학부) | Hwa Woon Lee (Division of Earth Environmental System, Pusan National University) Corresponding author