지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학술대회자료
- 저자정보
- 발행연도
- 2007.10
- 수록면
- 28 - 32 (5page)
이용수
초록· 키워드
오류제보하기
The focus in this paper is on the outer wind structure and structure changes in tropical cyclones. Deviations from traditional wind profiles with radius will occur when secondary eyewalls form, and a recent high-resolution numerical simulation by Terwey and Montgomery (2007) suggests large increases in the radius of 50 kt (R??) and 35 kt (R₃?) winds as a result of a secondary eyewall. Creation of the conditions for an annular hurricane would also imply a large increase in R?? and R₃?. A unique set of H*Wind analyses of the surface wind in the Atlantic during the 2003-2005 seasons is examined to evaluate outer wind structure (R₃₄ and R??) changes. Whereas a small set of H*Wind analyses during the formation stage has the expected increases in R₃₄ values, a considerable percentage of R₃₄ decreases occur during the intensification stages when only increases would be expected. Similarly, a considerable percentage of R₃₄ increases are observed during the decay phase when decreases would be expected, although a forecaster rule-of-thumb is that the tropical cyclone circulation expands during the decay stage. The conclusion is that further study is required to understand the outer wind structure changes during the life cycle of the tropical cyclone. individual storm evolutions using the H*Wind analyses are presently being studied.
목차
ABSTRACT
1. Introduction
2. Track dependency on outer wind structure
3. More complex outer wind profiles
4. Idealizen versus actual tropical cyclone structure changes
Acknowledgements
REFERENCES
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