2017
DOI: 10.3390/w9040240
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Estimation of Probable Maximum Precipitation in Korea using a Regional Climate Model

Abstract: Extreme precipitation events have been extensively applied to the design of social infra structures. Thus, a method to more scientifically estimate the extreme event is required. This paper suggests a method to estimate the extreme precipitation in Korea using a regional climate model. First, several historical extreme events are identified and the most extreme event of Typhoon Rusa (2002) is selected. Second, the selected event is reconstructed through the Weather Research and Forecasting (WRF) model, one of … Show more

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Cited by 24 publications
(15 citation statements)
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“…The most extreme events are selected for consideration for flood forecasting in the Imjin River basin. In 2002, Typhoon Rusa ripped through South Korea in the Gangneung area between 31 August and 1 September, affecting the eastern and southern parts of Korea with almost 1000 mm of rainfall in 30 h [33,34]. The typhoon caused the submergence of 9000 houses and killed 113 people.…”
Section: Hydrological and Meteorological Datamentioning
confidence: 99%
“…The most extreme events are selected for consideration for flood forecasting in the Imjin River basin. In 2002, Typhoon Rusa ripped through South Korea in the Gangneung area between 31 August and 1 September, affecting the eastern and southern parts of Korea with almost 1000 mm of rainfall in 30 h [33,34]. The typhoon caused the submergence of 9000 houses and killed 113 people.…”
Section: Hydrological and Meteorological Datamentioning
confidence: 99%
“…ํŠนํžˆ, Ohara et al (2011) ๋ฐ Ishida et al (2015a, 2015b์˜ ์—ฐ๊ตฌ์—์„œ ๋ฌผ๋ฆฌ๊ธฐ๋ฐ˜ ์ˆ˜์น˜๊ธฐ์ƒ๋ชจํ˜• ์˜ ๋™์—ญํ•™์  ๋‹ค์šด์Šค์ผ€์ผ๋ง ๊ธฐ๋ฒ•์„ ์ด์šฉํ•˜์—ฌ ๊ธฐ์ƒ์š”์†Œ์˜ ์ด๋™, ์ƒ๋Œ€์Šต๋„์˜ ์ตœ๋Œ€ํ™”, ๊ธฐ์˜จ์˜ ์ฆ๊ฐ€ ๋“ฑ์„ ์กฐํ•ฉํ•˜์—ฌ ๊ฐ•์šฐ๋ฅผ ์ตœ๋Œ€ํ™” ํ•˜๋Š” ๋ฐฉ๋ฒ•์ด ๊ฐœ๋ฐœ๋˜์—ˆ๋‹ค. ๊ตญ๋‚ด์—์„œ๋„ ํƒœํ’ ๋ฃจ์‚ฌ(RUSA)๋ฅผ ๋Œ€ ์ƒ์œผ๋กœ ์ˆ˜์น˜๊ธฐ์ƒ๋ชจ๋ธ์ธ WRF (Weather Research and Forecast) ๋ชจํ˜•์„ ์ด์šฉํ•˜์—ฌ ๊ธฐ์ƒ์š”์†Œ์˜ ๋ณ€ํ™”๋ฅผ ํ†ตํ•ด PMP๋ฅผ ์‚ฐ์ •ํ•˜๋Š” ์—ฐ๊ตฌ๊ฐ€ ์ˆ˜ํ–‰๋˜์—ˆ๋‹ค (Lee et al, 2017). ์ด์™€ ๊ฐ™์€ ์—ฐ๊ตฌ๋“ค์€ ๋ชจ๋‘ ๊ณตํ†ต์ ์œผ๋กœ ๊ณผ๊ฑฐ ๋ฐœ์ƒํ•œ ๊ฐ•์šฐ์‚ฌ์ƒ์„ ์„ ํƒํ•˜๊ณ  ์žฌํ˜„ํ•œ ํ›„ ๋ชจํ˜•์˜ ์ดˆ๊ธฐ ๋ฐ ๊ฒฝ๊ณ„ ์กฐ๊ฑด์˜ ๊ธฐ์ƒ์š”์†Œ๋“ค์„ ๋ณ€๊ฒฝํ•˜์—ฌ ๊ฐ•์šฐ ๋ฅผ ์ตœ๋Œ€ํ™”ํ•˜๋Š” ๋ฐฉ๋ฒ•์„ ์ ์šฉํ•˜๊ณ  ์žˆ๋‹ค.…”
Section: ์„œ ๋ก unclassified
“…However, the projected future precipitation in the EAMC region is very difficult to attain credibility because it shows very large variability depending on what climate model is applied [26]. In fact, even when a model to reproduce typhoon-induced rainfall in the past is constructed, very different rainfall simulations are often obtained depending on how the physical options of the regional climate model are combined under the same initial conditions and boundary conditions [27,28]. Uncertainty of the climate model results weakens the reliability of future climate data (especially rainfall) composed of sub-daily resolution, and it is difficult to obtain the reliability of various future hydrological components derived by using a complex deterministic water balance model using such future uncertain climate data as input data [29].…”
Section: Introductionmentioning
confidence: 99%