The shortwave aerosol direct radiative forcing (SWARF) was analyzed using the Clouds and Earth’s Radiant Energy System (CERES) data in the East Asian region from 2001 to 2010. In the Yellow Sea and the Korean Peninsula, located in the leeward side of China, significantly negative high SWARF at the top of atmosphere (TOA) occurs due to the long-range transport of anthropogenic (e.g. sulphate) and natural aerosols (e.g. mineral dust) from the East Asian continent. Conversely, eastern China has much higher levels of SWARF at the surface (SFC) due to anthropogenically emitted aerosol than in the Yellow Sea and the Korean Peninsula. Since the radiative forcing of aerosols in the atmosphere are different in type, aerosol types were classified into sea salt+sulphate, smoke, sulphate and dust by using satellite data. The analysis on the SWARF by the classified aerosol types indicated that sulphate occupies a predominant portion of the atmosphere in the Yellow Sea and the Korean Peninsula in the summer. In particular, the annual averages of the summer TOA SWARF increased in the Yellow Sea and the Korean Peninsula from 2001 to 2010.

Abstract
 1. 서 론
 2. 자료 및 방법
  2.1. 분석 대상 지역
  2.2. 분석 자료
 3. 결과 및 논의
  3.1. 동아시아 지역의 에어로졸 공간 분포
  3.2. 동아시아 지역에서 에어로졸 단파직접복사강제력의분포
  3.3. 동아시아 지역 에어로졸 단파직접복사강제력의 장기간변화
 4. 결 론
 참 고 문 헌

• 정지현(한국교원대학교 지구과학교육과) | Ji-Hyun Jeong (Department of Earth Science Education, Korea National University of Education)
• 김학성(한국교원대학교 지구과학교육과) | Hak-Sung Kim (Department of Earth Science Education, Korea National University of Education) Corresponding author
• 김준태(한국교원대학교 지구과학교육과) | Joon-Tae Kim (Department of Earth Science Education, Korea National University of Education)
• 박용필(한국교원대학교 지구과학교육과) | Yong-Pil Park (Department of Earth Science Education, Korea National University of Education)
• 최현정(한국과학영재학교) | Hyun-Jung Choi (Korea Science Academy of KAIST)