The 40~50Day Intraseasonal Oscillation of the Geostationary Meteorological Satellite High Cloud Amount

GMS 상층운량의 40~50일 계절만 진동

  • 하경자 (부산대학교 컴퓨터 및 정보통신연구소) ;
  • 서애숙 (부산대학교 대기과학과, 기상연구소 원격탐사연구실, 일본 동해대학 해양학부)
  • Published : 1996.10.01

Abstract

Intraseasonal variability of the tropical convection over the Indian/western Pacific is studied using the Geostationary Meteorological Satellite high cloud amount. This study is directed to find the tropical-extratropical interaction in the frequency range of intraseasonal and interannual variabilities of the summer monsoon occured over the domain of 90E-171W and 495-50N. Especially, in order to investigate the intraseasonal interaction of last Asia summer monsoon associated with the tropical convections in the high cloud amounts, the spatial and time structure of the intraseasonal oscillation for the movement-and the evolution of the large-scale connections are studied. To describe the spatial and the time evolution, the extended empirical orthogonal function analysis is applied. The first mode may be considered to a normal structure, indicating that the strong convection band over 90E-120E is extended to sastward but this mode was detected as the intraseasonal variability during summer monsoon. It is found that the dominant intraseasonal mode of the tropical convection consists of the spatial changes over a broad period range centered around 40~50days.

인도양 및 서태평양 부근의 적도 대류의 계절안 변동을 GMS 상층운량을 사용하여 연구되었다. 이 연구는 90E-l7IW와 495-5ON 영역에서의 여름 몬순의 계절안 및 경년 변동 주기내의 열대-중위도 상호 관계를 찾는데 방향이 맞추어져 있다. 특히 상층운량에서 적도 대류와 연관된 동아시아 몬순의 계절안 상호작용을 이해하기 위해 대규모 대류의 이동과 진화에 대한 공간 및 시간 구조의 분석이 이루어졌다. 공간과 시간 발전을 동시에 보기 위해 연장 경험적 직교함수 분석이 적용되었다. 그 첫째는 정규 구조로 간주될 수 있는, 90E-l2OE의 강한 대류의 동쪽 확장이 뚜렷한 모드이나 우리나라와 일본 부근에서는 해마다 변동하는 모드이다. 둘째, 세째 및 네째 모드들은 여름 몬순 동안 계절안 변동성을 가지고 증폭되는 모드들이다. 적도 대류에서 가장 강력한 계절안 모드가 바로 40~50일 부근에 탁월 주기를 갖고 있는 공간 구조로 구성되는 것이 확인되었다.

Keywords

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