북한에 상륙한 태풍의 기후학적 특성
The Climatological Characteristics of the Landfall Typhoons on North Korea
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In this study, the climatological characteristics of the landfall typhoons on North Korea are surveyed to estimate the frequency, the intensity, the track, and their damage. The data for the period of 1951-2008 are used from both RSMC (Regional Specialized Meteorological Center) Tokyo Typhoon Center and NCEP/NCAR (National Centers for Environmental Prediction/National Center for Atmospheric Research), EM-DAT (Emergency Events Database). There are the ten highest frequencies from 1961 to 1965 and is one frequency for the period of both 1966-1979 and 1976-1980 respectively. Even if a clear trend on the frequency of typhoon is not defined, it is noticeable the intensity has been weak since the frequency of TS (Tropical Storm) decreased. In order to figure out both the characteristic of intensity and the relation between the typhoon track and the expansion of North Pacific High (NPH), Typhoon's tracks are classified into three types as follows: (I) landing on the west coast of North Korea through the mainland of China, (II) landing on the west coast of North Korea, (III) landing on a central/eastern part of the Korean peninsula through South Korea. More often than not, the characteristic of Type (I) is the case of a landfall after it becomes extratropical cyclone. Type(II) and Type(III) show a landfall as TS grade, by comparision. On the relation between the typhoon's track and the expansion of NPH analyzed, Type (I) shows the westward expansion while both Type (II) and Type (III) show the northward expansion and development of NPH. This means the intensity of a typhoon landfall on North Korea is variable depending on the development of NPH. Finally,only two cases are found among total five cases in EM-DAT, reportedly that North Korea was damaged. And therefore, the damage by the wind of Prapiroon (the 12th typhoon, 2000) and heavy rainfall with Rusa (the 15th typhoon, 2002) landing on North Korea was analyzed. Moreover, it is estimated both Prapiroon and Rusa have done badly damaged to North Korea as the economical losses of as much as six billion and five hundred-thousand US dollar, respectively. Climatological characteristics, Landfall Typhoon, North Korea
Abstract
In this study, the climatological characteristics of the landfall typhoons on North Korea are surveyed to estimate the frequency, the intensity, the track, and their damage. The data for the period of 1951-2008 are used from both RSMC (Regional Specialized Meteorological Center) Tokyo Typhoon Center and NCEP/NCAR (National Centers for Environmental Prediction/National Center for Atmospheric Research), EM-DAT (Emergency Events Database). There are the ten highest frequencies from 1961 to 1965 and is one frequency for the period of both 1966-1979 and 1976-1980 respectively. Even if a clear trend on the frequency of typhoon is not defined, it is noticeable the intensity has been weak since the frequency of TS (Tropical Storm) decreased. In order to figure out both the characteristic of intensity and the relation between the typhoon track and the expansion of North Pacific High (NPH), Typhoon's tracks are classified into three types as follows: (I) landing on the west coast of North Korea through the mainland of China, (II) landing on the west coast of North Korea, (III) landing on a central/eastern part of the Korean peninsula through South Korea. More often than not, the characteristic of Type (I) is the case of a landfall after it becomes extratropical cyclone. Type(II) and Type(III) show a landfall as TS grade, by comparision. On the relation between the typhoon's track and the expansion of NPH analyzed, Type (I) shows the westward expansion while both Type (II) and Type (III) show the northward expansion and development of NPH. This means the intensity of a typhoon landfall on North Korea is variable depending on the development of NPH. Finally,only two cases are found among total five cases in EM-DAT, reportedly that North Korea was damaged. And therefore, the damage by the wind of Prapiroon (the 12th typhoon, 2000) and heavy rainfall with Rusa (the 15th typhoon, 2002) landing on North Korea was analyzed. Moreover, it is estimated both Prapiroon and Rusa have done badly damaged to North Korea as the economical losses of as much as six billion and five hundred-thousand US dollar, respectively. Climatological characteristics, Landfall Typhoon, North Korea
참고문헌 (30)
- 북한 지리교육을 위한 초·중등학교 교수·학습자료 개발연구, "교육인적자원부", 238~ (2001)
- 권원태, "한반도 최근 10년 기후특성", 한국수자원학회 07 학술발표회 논문집, pp.278~280 (2007), 한국수자원학회
- 태풍백서, "기상청", 261~ (1996)
- 김정희, "2002년 15호 태풍 ‘루사’의 강수량 수치 모의", 대기, 13(1), pp.440~441 (2003)
- 김주홍, "벡터 EOF와 Fuzzy 군집을 이용한 여름철 태풍의 기후적 진로 유형 분류와 유형별 대규모 순환 패턴 분석", 대기, 13(1), pp.406~409 (2003)
- 북한의 자연재해취약지 추정 및 남북협력 방안 연구, "명수정", 한국환경정책·평가연구원, 175~ (2008)
- 박관영, "기상재해와 대책", 기술사, 41(4), pp.36~43 (2008)
- 남북 자연재해방지 공동협력 성과 도출을 위한 전략에 관한 정책연구, "박순웅", 기상청, 151~ (2007)
- 박종길, "한반도에 영향을 주는 태풍의 통계적 특성변화", 대기, 16(1), pp.1~17 (2006)
- 박종길, "우리나라의 태풍에 의한 강수의 특성", 한국기상학회지, 25(2), pp.45~55 (1989)
- 박 종 길, "한반도에서 발생되는 기상재해 분석", 한국환경과학회지, 14(6), pp.613~619 (2005), 한국환경과학회
- 설동일, "태풍에 의한 우리나라의 기상재해에 관한 통계적 연구", 한국항해학회지, 14(4), pp.47~54 (1992)
- 안숙희, "한반도 영향 태풍의 이동경로에 따른 재해특성", 한국방재학회논문집, 8(3), pp.29~36 (2008), 한국방재학회
- 통일대비 남북한 기상업무 협력방안과 기상청의 역할 모색, "오재호", 과학기술정책연구원, 104~190 (1999)
- 이호만, "2000년 여름 한반도 연안 폭풍해일 연구", 대기, 11(1), pp.108~112 (2001)
- 이동규, "한반도에 접근하는 태풍, 1960-1989 제1부 : 통계와 종관 개요", 한국기상학회지, 28(2), pp.133~147 (1992)
- 정병석, "2002년 제15호 태풍“루사”에 의하여 야기된 영동지방 호우 분석", 대기, 12(3), pp.414~417 (2002)
- 정용승, "북한의 과학기술-기상ㆍ대기현상의 연구현황", 과학과 기술, 26(10), pp.83~85 (1993)
- 정용승, "남북한의 기상·대기환경과학 비교", 과학과 기술, 27(1), pp.49~52 (1994)
- Ki-Seon Choi, "Climatological Characteristics of Tropical Cyclones Making Landfall over the Korean Peninsula", 한국기상학회지, 43(2), pp.97~109 (2007), 한국기상학회
- Choi, K. S., "Cluster analysis of tropical cyclones making landfall on the Korean Peninsula", Adv. Atmos. Sci, 26(2), pp.202~210 (2009)
- Emanuel, K., "Increasing destructiveness of tropical cyclones over the past 30 years", Nature, 436, pp.686~688 (2005)
- Germanwatch, "Weatherrelated loss events and their impacts on countries in 2007 and in a long-term comparison", Global Climate Risk Index 2009 (2008)
- Hui, Y. U., "Comparison of three tropical cyclone intensity dataset", Acta. Meteor. Sin., 21, pp.121~128 (2007)
- IPCC, "Climate Change 2007: Impacts, Adaptation and Vulnerability. Working Group II contribution to the fourth assessment report of the intergovernmental panel on climate change" (2007), Cambridge University Press
- Kamahori, H., "Variability in intense tropical cyclone days in the western North Pacific", Sci. Online Lett. Atmos., 2, pp.104~107 (2006)
- Kenneth, R. K., "The International Best Track Archive for Climate Stewardship (IBTrACS)", Bull. Amer. Meteor. Soc., 91(3), pp.363~376 (2010)
- H. Joe Kwon, "Climatological Differences between the Two Typhoon Centers' Tropical Cyclone Information in the Western North Pacific", 한국기상학회지, 42(3), pp.183~192 (2006), 한국기상학회
- "Voice of America, 2007", 12, ~
- Webster P. J., "Changes in Tropical Cyclone Number, Duration, and Intensity in a Warming Environment", Science, 309, pp.1844~1846 (2005)