RISS 학술연구정보서비스

검색
다국어 입력

http://chineseinput.net/에서 pinyin(병음)방식으로 중국어를 변환할 수 있습니다.

변환된 중국어를 복사하여 사용하시면 됩니다.

예시)
  • 中文 을 입력하시려면 zhongwen을 입력하시고 space를누르시면됩니다.
  • 北京 을 입력하시려면 beijing을 입력하시고 space를 누르시면 됩니다.
닫기
    인기검색어 순위 펼치기

    RISS 인기검색어

      CASES-99 자료를 이용한 안정한 대기상태에서의 상사 관계의 평가 = (An) Evaluation of similarity relationships using CASES-99 in the stable boundary layer

      한글로보기

      https://www.riss.kr/link?id=T10026597

      • 0

        상세조회
      • 0

        다운로드
      서지정보 열기
      • 내보내기
      • 내책장담기
      • 공유하기
      • 오류접수

      부가정보

      다국어 초록 (Multilingual Abstract) kakao i 다국어 번역

      Monin-Obukhov similarity theory during the stable boundary layer(SBL) is evaluated in terms of stability and large-scale environment using the CASES-99 field campaign data. Based on similarity theory, flux-profile relations, intermittency, and turbulent statistics are examined and various features of different stability regimes under the stable condition are discussed. Monin-Obukhov similarity was generally derived from Buckingham Pi theory, as a function of a stability parameter z/L and a dimensionless function ø. Basically, similarity formulas are based on a stationary atmospheric surface layer over horizontally homogeneous terrain. In this paper, for large scale forcing three types of "strong", "weak" and "normal" wind are used for the criterion of mean wind condition.
      From occurrence frequency of z/L, where L is the Monin-Obukhov length, the weakly stable case of 0.01< z/L <0.1 and the strong stratification of z/L>1 are concentrated in the strong and weak wind condition. For z-less concept, the mixing length is well agreed with observation. Dimensionless wind shear ø_(m) is generally agreed with formula proposed by Businger et al. (1971) and Beljaars and Holtslag (1991) where z/L is less than 1 for the normal wind case. For the weak wind case and strong stability were z/L > 1, the relationships between parameterized formula and calculated value from observation, and similarity theory break down. Flux intermittency of turbulence might be a good index for the different stability regimes except the strong wind condition.
      번역하기

      Monin-Obukhov similarity theory during the stable boundary layer(SBL) is evaluated in terms of stability and large-scale environment using the CASES-99 field campaign data. Based on similarity theory, flux-profile relations, intermittency, and turbule...

      Monin-Obukhov similarity theory during the stable boundary layer(SBL) is evaluated in terms of stability and large-scale environment using the CASES-99 field campaign data. Based on similarity theory, flux-profile relations, intermittency, and turbulent statistics are examined and various features of different stability regimes under the stable condition are discussed. Monin-Obukhov similarity was generally derived from Buckingham Pi theory, as a function of a stability parameter z/L and a dimensionless function ø. Basically, similarity formulas are based on a stationary atmospheric surface layer over horizontally homogeneous terrain. In this paper, for large scale forcing three types of "strong", "weak" and "normal" wind are used for the criterion of mean wind condition.
      From occurrence frequency of z/L, where L is the Monin-Obukhov length, the weakly stable case of 0.01< z/L <0.1 and the strong stratification of z/L>1 are concentrated in the strong and weak wind condition. For z-less concept, the mixing length is well agreed with observation. Dimensionless wind shear ø_(m) is generally agreed with formula proposed by Businger et al. (1971) and Beljaars and Holtslag (1991) where z/L is less than 1 for the normal wind case. For the weak wind case and strong stability were z/L > 1, the relationships between parameterized formula and calculated value from observation, and similarity theory break down. Flux intermittency of turbulence might be a good index for the different stability regimes except the strong wind condition.

      더보기

      목차 (Table of Contents)

      • 목차 = Ⅰ
      • 제1장 서론 = 1
      • 제2장 자료 = 6
      • 제3장 기본장 (온도와 바람)의 추이와 분류 = 8
      • 3.1 온도와 바람장의 추이 = 8
      • 목차 = Ⅰ
      • 제1장 서론 = 1
      • 제2장 자료 = 6
      • 제3장 기본장 (온도와 바람)의 추이와 분류 = 8
      • 3.1 온도와 바람장의 추이 = 8
      • 3.2 종관장 분류 = 10
      • 제4장 상사관계의 매개 변수들 = 12
      • 4.1 모닝-오부코프 길이와 안정도 파라메타 = 12
      • 4.2 무차원 변수들 = 19
      • 4.2.1 리처드슨 수 = 19
      • 4.2.2 프란틀 수 = 24
      • 4.3 Z-less 접근과 혼합 길이 = 26
      • 제5장 플러스 프로파일 함수로 본 M-O 상사관계의 검증 = 29
      • 5.1 플럭스 프로파일 함수 = 29
      • 5.2 플럭스 프로파일 함수의 로그-선형 프로파일 = 36
      • 5.2.1 적분 바람 프로파일 = 36
      • 5.2.2 적분 온도 프로파일 = 41
      • 제6장 난류 통계 = 43
      • 6.1 마찰속도와 부력 플럭스 = 43
      • 6.2 난류의 단속성 = 49
      • 6.3 난류의 상관관계 = 52
      • 제7장 결론 = 54
      • 참고 문헌 = 57
      • Abstract = 61
      더보기

      분석정보

      View

      상세정보조회

      0

      Usage

      원문다운로드

      0

      대출신청

      0

      복사신청

      0

      EDDS신청

      0

      동일 주제 내 활용도 TOP

      더보기

      주제

      연도별 연구동향

      연도별 활용동향

      연관논문

      연구자 네트워크맵

      공동연구자 (7)

      유사연구자 (20) 활용도상위20명

      이 자료와 함께 이용한 RISS 자료

      나만을 위한 추천자료

      해외이동버튼