In this study the AWS was installed in three areas to analyze creation and characteristics of local wind circulation through observation. According to the result, in night time when mountain wind is well developed showed temperature in A area located in Dalbigol valley and B area adjacent with the valley was lower than C area located in the lowland of the center of city by 1.5∼4℃. The wind speed was also shown two times stronger than C area. In addition, in terms of wind direction, A and B areas showed east wind consistently according to topographic shapes of Dalbigol valley with high altitude and residential sites of lowland with low altitude.
Although the C area didn’t show big changes in wind direction due to the effects of city structures, east wind is often seen so mountain wind from Dalbigol valley is found to have an effect at least. Through the analysis of temperature, wind speed, and wind direction, nigh time showed relatively cold mountain wind blew following Dalbigol valley, throughout residential sites and to the center of city with lowland. During the daytime, the temperature in the city with lowland and residential sites is constantly higher than A area located in Dalbigol valley, and strong wind speed following Dalbigol valley, and three areas have 200∼300° of main wind direction, so west valley wind throughout the city with lowland and following Dalbigol is clearly formed.

Abstract
 1. 서 론
 2. 연구대상지역
 3. 연구방법
  3.1. 기상관측
  3.2. 국지풍 순환경로 파악을 위한 Envi-met 수치실험
 4. 결과 및 고찰
  4.1. 지상의 기상일변화
  4.2. 수치모델 결과
 5. 결 론
 참 고 문 헌

• 박명희(국립수산과학원) | Myong-Hee Park (National fisheries Research & Development Institute)
• 정우식(인제대학교 대기환경정보공학과/대기환경정보연구센터) | Woo-Sik Jung (Department of Atmospheric Environment Information Engineering/Atmospheric Environment Information Research Center, Inje University)
• 김해동(계명대학교 환경대학) | Hae-Dong Kim (College of Environment, Keimyung University) Corresponding Author