• Title/Summary/Keyword: 가뭄심도-지속기간-생기빈도 곡선

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Derivation of Drought Severity-Duration-Frequency Curves Using Drought Frequency Analysis (가뭄빈도해석을 통한 가뭄심도-지속시간-생기빈도 곡선의 유도)

  • Lee, Joo-Heon;Kim, Chang-Joo
    • Journal of Korea Water Resources Association
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    • v.44 no.11
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    • pp.889-902
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    • 2011
  • In this study, frequency analysis using drought index had implemented for the derivation of drought severity-duration-frequency (SDF) curves to enable quantitative evaluations of past historical droughts having been occurred in Korean Peninsular. Seoul, Daejeon, Daegu, Gwangju, and Busan weather stations were selected and precipitation data during 1974~2010 (37 years) was used for the calculation of Standardized Precipitation Index (SPI) and frequency analysis. Based on the results of goodness of fit test on the probability distribution, Generalized Extreme Value (GEV) was selected as most suitable probability distribution for the drought frequency analysis using SPI. This study can suggest return periods for historical major drought events by using newrly derived SDF curves for each stations. In case of 1994~1995 droughts which had focused on southern part of Korea. SDF curves of Gwangju weather station showed 50~100 years of return period and Busan station showed 100~200 years of return period. Besides, in case of 1988~1989 droughts, SDF of Seoul weather station were appeared as having return periods of 300 years.

Drought Analysis using SC-PDSI and Derivation of Drought Severity-Duration-Frequency Curves in North Korea (SC-PDSI를 이용한 북한지역 가뭄분석 및 가뭄심도-지속기간-생기빈도 곡선의 유도)

  • Kang, Shin Uk;Moon, Jang Won
    • Journal of Korea Water Resources Association
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    • v.47 no.9
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    • pp.813-824
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    • 2014
  • In this study, drought of North Korea are analyzed using drought index. 27 weather stations are selected and monthly precipitation and average temperature data are collected for drought analysis. SC-PDSI is used for drought analysis and calculated using collected weather data during 1984~2013 (30 years) in 27 weather stations. From the analysis result of historical drought event using drought index, it is confirmed that severe droughts occurred in the early and mid 2000's at most stations. Secondly, drought frequency analysis was carried out for the derivation of drought severity-duration-frequency (SDF) curves to enable quantitative evaluations of past historical droughts having been occurred in 6 stations (Pyeongyang, Hamheung, Cheongjin, Wonsan, Haeju, Sinuiju). This study can suggest return periods for historical major drought events by using derived SDF curves for each station. In the result, drought events in the early and mid 2000's had return periods of 20~50 years.

Analysis on the Spatio-Temporal Distribution of Drought using Potential Drought Hazard Map (가뭄우심도를 활용한 가뭄의 시공간적 분포특성분석)

  • Lee, Joo Heon;Cho, Kyeong Joon;Kim, Chang Joo;Park, Min Jae
    • Journal of Korea Water Resources Association
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    • v.45 no.10
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    • pp.983-995
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    • 2012
  • In this study, it was intended to analyze the spatio-temporal distribution of historical drought events occurred in Korea by way of drought frequency analysis using SPI (Standardized Precipitation Index), and Drought spell was executed to estimate drought frequency as per drought severity and regions. Also, SDF (severity-duration-frequency) curves were prepared per each weather stations to estimate spatial distribution characteristics for the severe drought areas of Korea, and Potential Drought Hazard Map was prepared based on the derived SDF curves. Drought frequency analysis per drought stage revealed that severe drought as well as extreme drought frequency were prominently high at Geum River, Nakdong River, and Seomjin River basin as can be seen from SDF curves, and drought severity was found as severer per each drought return period in the data located at Geum River, Nakdong River, and Seomjin River basins as compared with that of Seoul weather station at Han River basin. In the Potential Drought Hazard Map, it showed that Geum River, Seomjin River, and Yeongsan River basins were drought vulnerable areas as compared to upper streams of Nakdong River basin and Han River basin, and showed similar result in drought frequency per drought stage. Drought was occurred frequently during spring seasons with tendency of frequent short drought spell as indicated in Potential Drought Hazard Map of different season.