지원사업
학술연구/단체지원/교육 등 연구자 활동을 지속하도록 DBpia가 지원하고 있어요.
커뮤니티
연구자들이 자신의 연구와 전문성을 널리 알리고, 새로운 협력의 기회를 만들 수 있는 네트워킹 공간이에요.
논문 기본 정보
- 자료유형
- 학위논문
- 저자정보
- 지도교수
- 변희룡
- 발행연도
- 2013
- 저작권
- 부경대학교 논문은 저작권에 의해 보호받습니다.
이용수0
이 논문의 연구 히스토리 (2)
- 이 논문의 후속연구가 궁금하신가요?
- 연관 학술논문 또는 학술발표를 통해 보다 발전된 연구결과를 확인하실 수 있습니다.
- 이 논문의 연구 히스토리 확인하기
초록· 키워드
오류제보하기
This study investigated the spatial distribution and long-term variations of the latest frost days (LFD) and analyzed synoptically for the cause of occurrences in Korea. The average LFD in Korea during the period of modern observation (1905~2011) were experienced at the earliest in Masan (March 13) and the latest in Daegwallyeong (May 7). The interannual variations of LFD tend to be earlier (-0.21 days year-1) from 1971 to 2011, the largest change in value was shown in Wonju (-0.69 days year-1). LFD has recorded 138 times in the ancient literature (The Annals of the Joseon Dynasty:1392~1904), and they are most concentrated in May (40%).
As a result of comparison with synoptic characteristics of LFD between in the latest 5 years and in the earliest 5 years, LFD in the latest 5years show lower temperature than in the earliest 5 years. It is because the southerly inflow from North Pacific and near the equator was weaker in late years than in early years. LFD in Daegwallyeong (June 2, 2010) is the latest by low temperatures and high humidity during modern observation period. It is because cold air in the upper level inflow in to the Korean peninsula by the blocking high occurred in China and inflow paths of southward wind were moved to the West Sea from the East Sea of Korea, as the anticyclone occurred in the Sea of Okhotsk moved in southerly direction.
As a result of comparison with synoptic characteristics of LFD between in the latest 5 years and in the earliest 5 years, LFD in the latest 5years show lower temperature than in the earliest 5 years. It is because the southerly inflow from North Pacific and near the equator was weaker in late years than in early years. LFD in Daegwallyeong (June 2, 2010) is the latest by low temperatures and high humidity during modern observation period. It is because cold air in the upper level inflow in to the Korean peninsula by the blocking high occurred in China and inflow paths of southward wind were moved to the West Sea from the East Sea of Korea, as the anticyclone occurred in the Sea of Okhotsk moved in southerly direction.
목차
Contents iList of Figures iiList of Tables vAbstract vi1. 서론 12. 자료 및 분석 32.1 현대관측자료 32.2 고대문헌자료 83. 끝서리일의 변동 특징 93.1 평균 끝서리일의 공간분포 93.2 끝서리일의 시간적 변화경향 113.3 고대문헌자료와 비교 154. 끝서리일의 변동 원인 174.1 지리적 영향에 의한 끝서리일 변동 174.2 남풍 유입량에 의한 변동 214.3 가장 늦은 끝서리일 사례분석 275. 요약 및 결론 35Reference 37
최근 본 자료
댓글(0)
0