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    RISS 인기검색어

      Natural Variability and Warming Signals in Global Ocean Wave Climates

      한글로보기

      https://www.riss.kr/link?id=O106867392

      • 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.]

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        • 이화여자대학교 중앙도서관  
        • 고려대학교 도서관  
      • ⓒ COPYRIGHT THE BRITISH LIBRARY BOARD: ALL RIGHT RESERVED
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      다국어 초록 (Multilingual Abstract)

      This paper presents a multivariate classification of the global wave climate into types driven by atmospheric circulation patterns. The primary source of the net long‐term variability is evaluated based on historical wave simulations. Results show that the monsoon, extratropical, subtropical, and polar wave climate types of the Pacific and North Atlantic Oceans are dominated by natural variability, whereas the extratropical and subtropical wave climate types in the Indian Ocean, and the tropical wave climate types of the Atlantic and Pacific Oceans exhibit a global warming signal. In the Pacific sector of the Southern Ocean, strong natural variability may mask a global warming signal that is yet to emerge as being statistically significant. In addition, wave climate teleconnections were found across the world that can provide a framework for joint strategies to achieve the goals of climate adaption for resilient coastal communities and environments.
      Near‐surface wind systems drive global ocean wave conditions that are usually studied at regional or local scale. However, analyzing these relationships at the global scale is important to understand how natural climate oscillations, such as El Niño‐Southern Oscillation, and global warming, impact wave climate. Here we identify the large wave climates in homology to the climate regions (e.g., Tropical, Temperate, Polar) and are originated by the planetary wind systems. The results show that global warming signals have already emerged in the Indian Ocean and the tropical regions of the Pacific and Atlantic basins. In contrast, in the other ocean basins, natural variability is still the dominant signal and could mask global warming signals.



      The global ocean wave climate is classified into types according to the planetary wind systems responsible for their genesis

      In general, natural variability is shown to be the principal signal in wave climate types over the past 34 years

      Signals showing global warming have already emerged in the Indian Ocean, and the tropical regions of the Atlantic and Pacific Oceans


      The global ocean wave climate is classified into types according to the planetary wind systems responsible for their genesis
      In general, natural variability is shown to be the principal signal in wave climate types over the past 34 years
      Signals showing global warming have already emerged in the Indian Ocean, and the tropical regions of the Atlantic and Pacific Oceans
      번역하기

      This paper presents a multivariate classification of the global wave climate into types driven by atmospheric circulation patterns. The primary source of the net long‐term variability is evaluated based on historical wave simulations. Results show t...

      This paper presents a multivariate classification of the global wave climate into types driven by atmospheric circulation patterns. The primary source of the net long‐term variability is evaluated based on historical wave simulations. Results show that the monsoon, extratropical, subtropical, and polar wave climate types of the Pacific and North Atlantic Oceans are dominated by natural variability, whereas the extratropical and subtropical wave climate types in the Indian Ocean, and the tropical wave climate types of the Atlantic and Pacific Oceans exhibit a global warming signal. In the Pacific sector of the Southern Ocean, strong natural variability may mask a global warming signal that is yet to emerge as being statistically significant. In addition, wave climate teleconnections were found across the world that can provide a framework for joint strategies to achieve the goals of climate adaption for resilient coastal communities and environments.
      Near‐surface wind systems drive global ocean wave conditions that are usually studied at regional or local scale. However, analyzing these relationships at the global scale is important to understand how natural climate oscillations, such as El Niño‐Southern Oscillation, and global warming, impact wave climate. Here we identify the large wave climates in homology to the climate regions (e.g., Tropical, Temperate, Polar) and are originated by the planetary wind systems. The results show that global warming signals have already emerged in the Indian Ocean and the tropical regions of the Pacific and Atlantic basins. In contrast, in the other ocean basins, natural variability is still the dominant signal and could mask global warming signals.



      The global ocean wave climate is classified into types according to the planetary wind systems responsible for their genesis

      In general, natural variability is shown to be the principal signal in wave climate types over the past 34 years

      Signals showing global warming have already emerged in the Indian Ocean, and the tropical regions of the Atlantic and Pacific Oceans


      The global ocean wave climate is classified into types according to the planetary wind systems responsible for their genesis
      In general, natural variability is shown to be the principal signal in wave climate types over the past 34 years
      Signals showing global warming have already emerged in the Indian Ocean, and the tropical regions of the Atlantic and Pacific Oceans

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