KOREASCHOLAR

During a month, wave observation was characteristic of Suyuong bay since 16th of July. During the period, typhoons which were "Ma-on, Muifa" landed on Suyong bay. Observation point places a half-way point between Gwangan light beacon in the utmost bounds of the west and Haeundae floating buoy in east. The observation point was selected for confirming the relations of river discharge and storm surge of suyong bay. To investigate the characteristic, using meteorological data not in just Gwangan light beacon but in Haeundae floating buoy. As a result, at Gwangan light beacon the maximum significant wave observed was 3.5 m and period was 10,3 sec, at the Observation point each outcomes were 3.8 m and 10.1 sec, Haeundae floating had 2 m and 8.5 sec as consequences. The height of observation point was higher than Haeundae's or Gwangan’s and had two peaks. Although the wave direction in observation point came from southern east, being irregular in Haeundae floating buoy. Up to now, the interrelationship of weather conditions and wave characteristics have been verified, the characteristic of wave distribution

ABSTRACT
 1. 서 론
 2. 재료 및 방법
 3. 파랑분포 분석 결과
  3.1 계측된 파랑자료 분석 및 해양관측지점과의 비교
  3.2 태풍별 파랑분포 특성 분석
 4. 결론 및 요약
 참고문헌

• 김동환(부경대학교 해양공학과)
• 유창일(해양산업개발연구소) | C.I. Yoo (Research Center for Ocean Industrial Development(RCOID), Pukyong National University),)
• 김헌태(부경대학교 해양공학과) | H.T. Kim (Department of Ocean Engineering, Pukyong National University)
• 류청로(부경대학교 해양공학과) | C.R. Ryu (Department of Ocean Engineering, Pukyong National University)