논문 상세보기

남한 지역의 홀로세 중후기 기후변화 KCI 등재

  • 언어KOR
  • URLhttps://db.koreascholar.com/Article/Detail/43746
  • DOIhttps://doi.org/10.14383/cri.2013.8.2.127
서비스가 종료되어 열람이 제한될 수 있습니다.
기후연구 (Journal of Climate Research)
건국대학교 기후연구소 (KU Climate Research Institute)
초록

There is not much difference in mid- to late-Holocene climate change between in South Korea and in other parts of the northern hemisphere. According to paleoclimate data from South Korea, the Holocene Climate Optimum ended around 7600-6000 BP. Lower latitudinal areas seemingly showed later termination times of the Holocene Climate Optimum. In late-Holocene, the climate was relatively cool between AD 200-AD 800 and AD 1300-AD 1900 and relatively warm between AD 800-AD 1300. In addition, the climate might be relatively cool between 1200 BC-400 BC and relatively warm between 400 BC-AD 200.

목차
Abstract 1. 서론 2. 홀로세 중기 기후-한반도의 홀로세 기후(몬순) 최적기는? 3. 홀로세 후기 기후 4. 요약 및 결론 참고문헌
저자
  • 박정재