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논문 기본 정보
- 자료유형
- 학술저널
- 저자정보
- 저널정보
- 한국기상학회 Asia-Pacific Journal of Atmospheric Sciences Journal of the Korean Meteorological Society Vol.42 No.1
- 발행연도
- 2006.2
- 수록면
- 41 - 55 (15page)
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초록· 키워드
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The 1/2° Ocean General Circulation Model (OGCM) is utilized to study the annual variability of temperature in the North Pacific. The comparison between this model and observation shows almost constant phase features of 200 m and 400 m temperature in the northwestern Pacific Ocean. Thus, we can induce that the annual signal of a westward progressive Rossby waves in the eastern midlatitude region of the North Pacific is not found in western part of that. In 20°N longitude line of 400 m temperature simulated by the model, the phase of the eastern region of 170°E shows progressive wave characteristics and that of western region of 170°E is almost constant 140°. In this paper, we explain the reason of these different patterns in the midlatitude using a simple solution of quasi geostrophic equation including dissipation effect and model results.
목차
Abstract
1. Introduction
2. Model
3. Annual variability of temperature in the North Pacific Ocean
4. Rossby wave propagation with dissipation effect
5. Comparison of annual variability between the model and observation in the northwestern Pacific Ocean
6. Summary and Conclusion
Acknowledgements
REFERENCE
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UCI(KEPA) : I410-ECN-0101-2009-453-016239029