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      Relationships Between the Typhoon‐Induced Wind and Waves in the Northern South China Sea

      한글로보기

      https://www.riss.kr/link?id=O106438789

      • 저자
      • 발행기관
      • 학술지명
      • 권호사항
      • 발행연도

        2021년

      • 작성언어

        -

      • Print ISSN

        0094-8276

      • Online ISSN

        1944-8007

      • 등재정보

        SCI;SCIE;SCOPUS

      • 자료형태

        학술저널

      • 수록면

        n/a-n/a   [※수록면이 p5 이하이면, Review, Columns, Editor's Note, Abstract 등일 경우가 있습니다.]

      • 소장기관
      • 구독기관
        • 전북대학교 중앙도서관  
        • 성균관대학교 중앙학술정보관  
        • 부산대학교 중앙도서관  
        • 전남대학교 중앙도서관  
        • 제주대학교 중앙도서관  
        • 중앙대학교 서울캠퍼스 중앙도서관  
        • 인천대학교 학산도서관  
        • 숙명여자대학교 중앙도서관  
        • 서강대학교 로욜라중앙도서관  
        • 계명대학교 동산도서관  
        • 충남대학교 중앙도서관  
        • 한양대학교 백남학술정보관  
        • 이화여자대학교 중앙도서관  
        • 고려대학교 도서관  
      • ⓒ COPYRIGHT THE BRITISH LIBRARY BOARD: ALL RIGHT RESERVED
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      다국어 초록 (Multilingual Abstract)

      Wind‐wave interactions have been broadly investigated for their great implications on air‐sea momentum transfer, whereas our knowledge on those forced by typhoons (hurricanes) is still limited. Accordingly, relationships between wind and wave characteristics were analyzed using observations on the northern South China Sea during four typhoons. An empirical wind‐wave model was proposed for typhoon‐induced wind seas which exhibits satisfactory skills in predicting significant wave heights (Hs). Meanwhile, typhoon‐forced wind‐wave relation was investigated using the wave growth function. By delineating the relationship between the dimensionless Hs and peak wave period scaled with 10 m and friction wind velocities, simplified functions for the growing and steady wind seas were proposed, respectively. However, great misalignment could occur owing to the contamination of swells resulting from the typhoon's slow translation speed, as well as the extremely short or long radial distance from typhoon centers, indicating the necessity of considering typhoon structures in screening swell influences.
      Wind and waves interact with each other at the ocean surface, and such processes have significant impacts on oceanic and atmospheric dynamics. As our knowledge of typhoon‐forced wind waves is still limited, we investigated the wind‐wave relationship using buoy observations on the northern South China Sea. An empirical model was proposed for typhoon‐induced wind seas which exhibits satisfactory skills in predicting significant wave heights. Meanwhile, relationships between wind and wave characteristics of the growing and steady wind seas were derived using simplified wave growth functions. Such formulas could well estimate wind speed using observed wave characteristics, whereas errors could present with the contamination of swells, indicating the necessity of considering typhoon structures in screening swell influences.



      A wind‐wave model for typhoon‐induced growing wind seas is proposed based on a quadratic function

      The relationship between wind and wave characteristics was derived from simplified wave growth functions

      Typhoon structures should be considered for a more efficient screening of swells


      A wind‐wave model for typhoon‐induced growing wind seas is proposed based on a quadratic function
      The relationship between wind and wave characteristics was derived from simplified wave growth functions
      Typhoon structures should be considered for a more efficient screening of swells
      번역하기

      Wind‐wave interactions have been broadly investigated for their great implications on air‐sea momentum transfer, whereas our knowledge on those forced by typhoons (hurricanes) is still limited. Accordingly, relationships between wind and wave char...

      Wind‐wave interactions have been broadly investigated for their great implications on air‐sea momentum transfer, whereas our knowledge on those forced by typhoons (hurricanes) is still limited. Accordingly, relationships between wind and wave characteristics were analyzed using observations on the northern South China Sea during four typhoons. An empirical wind‐wave model was proposed for typhoon‐induced wind seas which exhibits satisfactory skills in predicting significant wave heights (Hs). Meanwhile, typhoon‐forced wind‐wave relation was investigated using the wave growth function. By delineating the relationship between the dimensionless Hs and peak wave period scaled with 10 m and friction wind velocities, simplified functions for the growing and steady wind seas were proposed, respectively. However, great misalignment could occur owing to the contamination of swells resulting from the typhoon's slow translation speed, as well as the extremely short or long radial distance from typhoon centers, indicating the necessity of considering typhoon structures in screening swell influences.
      Wind and waves interact with each other at the ocean surface, and such processes have significant impacts on oceanic and atmospheric dynamics. As our knowledge of typhoon‐forced wind waves is still limited, we investigated the wind‐wave relationship using buoy observations on the northern South China Sea. An empirical model was proposed for typhoon‐induced wind seas which exhibits satisfactory skills in predicting significant wave heights. Meanwhile, relationships between wind and wave characteristics of the growing and steady wind seas were derived using simplified wave growth functions. Such formulas could well estimate wind speed using observed wave characteristics, whereas errors could present with the contamination of swells, indicating the necessity of considering typhoon structures in screening swell influences.



      A wind‐wave model for typhoon‐induced growing wind seas is proposed based on a quadratic function

      The relationship between wind and wave characteristics was derived from simplified wave growth functions

      Typhoon structures should be considered for a more efficient screening of swells


      A wind‐wave model for typhoon‐induced growing wind seas is proposed based on a quadratic function
      The relationship between wind and wave characteristics was derived from simplified wave growth functions
      Typhoon structures should be considered for a more efficient screening of swells

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