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상당온위를 사용한 동아시아 여름철 몬순의 6월 및 7월 주 변동 모드 분석

Dominant Modes of the East Asian Summer Monsoon Using Equivalent Potential Temperature

  • 손준혁 (부산대학교 지구환경시스템학부 대기환경과학과) ;
  • 서경환 (부산대학교 지구환경시스템학부 대기환경과학과)
  • Son, Jun-Hyeok (Division of Earth Environmental System, Department of Atmospheric Sciences, Pusan National University) ;
  • Seo, Kyong-Hwan (Division of Earth Environmental System, Department of Atmospheric Sciences, Pusan National University)
  • 투고 : 2012.10.21
  • 심사 : 2012.12.19
  • 발행 : 2012.12.31

초록

The monsoon front lies on East Asian region, but it gradually propagates to the north during the boreal summer. The equivalent potential temperature (EPT) reveals the thermodynamical features of air masses and monsoon front. Therefore, this study considered the thermodynamical EPT and dynamical wind fields to clarify the peculiarity of East Asian summer monsoon (EASM) variations in June and July, respectively. Western North Pacific subtropical high (WNPSH) and Okhotsk sea high (OSH) both play the crucial role to interannual variations of EASM frontal activity and amount of rainfall. The OSH is important in June, but the WNPSH is key factor in July. Furthermore, the OSH (June) is affected by North Atlantic tripolar sea surface temperature (SST) pattern and WNPSH (July) is influenced by North Indian Ocean SST warming.

키워드

참고문헌

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피인용 문헌

  1. Analysis for Onset of Changma Using Ieodo Ocean Research Station Data vol.24, pp.2, 2014, https://doi.org/10.14191/Atmos.2014.24.2.189