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논문 기본 정보
- 자료유형
- 학술저널
- 저자정보
- 발행연도
- 2005.12
- 수록면
- 1,089 - 1,100 (12page)
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초록· 키워드
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In this study, we configurated and validated the ocean general circulation model, MOM3, in order to understand the propagation process of El Nino signals contained in subsurface oceanic parameters in the Pacific Ocean. Time-longitude diagram of the depth of the 20℃ isotherm and the disappearance of equatorial undercurrent during 1982-1983 El Nino event coincide with the observation evidences. From the EOF and composite analysis of heat content of the upper 300 meters, meridional exchange of water mass during El Nino evolution can be extracted from the second mode of EOF. Meridional redistribution of subsurface water mass occurs after the zonal advection of warm water from the western to eastern tropical Pacific in about one year. Consistent results are obtained for the depth of the 20℃ isotherm. Meridional exchange of water mass is also achieved by transport anomalies in the western boundary currents such as Kuroshio and New Guinea coastal current with an 8- to 13-month time delay on the interannual time scale.
목차
Abstract
1. 서론
2. 모델 개요
3. 모델 검증
4. 아표층 해양변수의 경년 변동
5. 요약 및 토의
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UCI(KEPA) : I410-ECN-0101-2009-453-016238926