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윤정수,황석환,강나래,이동률,이건행 한국수자원학회 2021 한국수자원학회논문집 Vol.54 No.12
강우레이더는 시공간적으로 높은 해상도의 레이더 강우를 제공하고 있으며, 이러한 레이더 강우는 초단기 예측 강우 모형의 입력자료로 활용 될 수 있다. 한국건설기술연구원은 레이더 강우로부터 추정된 초단기 예측 강우 자료를 활용하여 돌발홍수 예측 정보를 실시간으로 제공할 수 있는 돌발홍수 예측시스템을 개발하였다. 그러나 레이더 편파변수에 오차가 존재하는 경우 레이더 강우의 정확도는 낮게 나타날 수밖에 없으며, 이에 따라 초단기 예측 강우 자료의 정확도 역시도 낮게 나타날 수밖에 없다. 이에 본 연구에서는 레이더 강우의 정확도를 실시간으로 향상시키기 위해 레이더 편파변수 오차를 실시간으로 보정하는 프로그램을 개발하였다. 이를 위해 먼저 비슬산 레이더의 과거 363개의 강우사례에 편파변수 편의 보정에 따른 효과를 비실시간으로 검증하였다. 그 결과 편파변수의 오차 보정 시 레이더 강우의 정확도(1-NE) 수준은 약 70% 내외의 수준으로 나타났으며 상관계수는 0.8 이상으로 나타났다. 또한 실시간 편파변수 오차 보정 프로그램을 수행한 결과에서도 레이더 강우의 정확도(1-NE)를 약 70% 내외의 수준까지 향상시킬 수 있었다. Rain radar provides high spatio-temporal radar rainfall that can be used as input data to short-term precipitation forecasting models. Korea Institute of Civil Engineering and Building Technology (KICT) has developed a flash flood forecasting system that is providing flash flood forecasting based on short-term rainfall forecasts estimated by the radar rainfall. Accuracy of the radar rainfall as well as the short-term rainfall forecasts, however, can deteriorate when radar polarimetric variables have error. In this study, we develope real-time program that can correct the error inherent in the radar polarimetric variables. First, effect according to the correction of the error was verified using 363 rainfall events on non real-time. The accuracy (1-NE) of the radar rainfall was approximately 70% and correlation coefficient was higher than 0.8 after correcting the error on non real-time. The accuracy (1-NE) using the real-time program was also approximately 70% after correcting the error.
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윤정수,박상운,고윤영,오윤근 제주대학교 해양연구소 2000 해양자원연구소연구보고 Vol.24 No.-
The study area is situated between 31˚00' ~ 33˚30' N and 122˚30' ~126˚00' E as a part of the East China Sea continental shelf. The distribution of sediment in the study area can be classified three sedimentary types. Modern land derived muddy sediments consisting of silt and mud are distributed at mouth of the Changjiang River. and are also observed the southwest offshore of the Cheju Island. The sandsilt-clay miadre sediments are presented in the outer shelf area. The relict sand are distributed between the mordern and mixture sediment. The inner-shelf mud consisted of 8.89% sand. 59.05% silt. 32.06% clay and mean size of 6.90Φ. The offshore mud composed of 5.83% sand. 34.54% silt. 59.63% clay and mean size of 8.32). and also have higher water content and organic carbon. The C/N ratio showed higher in the inner-shelf mud (10.14) rather than that of the offshore mud (8.68). Most of the Changiiang River suspended matter is entrapped in the area around the Changjiang Estuary to the west of 123˚30' E. Only a small part of the suspended matter can be moved by Changjiang Diluted Plume to the southeastern and northeastern middle shelf. The higher suspended matter concentration gradient zone are observed in the northwest central region, and this plume zone separated from Changjiang Estuary by a low oncentration of less than 5 mg/ l or 15 mg/ l. The sediment accumulation rate in the inner shelf mud deposit near the mouth of the Changjiang River is 1.70 cm/yr and characterized by physical stratified mud. The sedimentation rate in the offshore mud deposit to the southwest of Cheju Island shows 0.28 cm/yr and characterized by homogenous mud. The difference in fine-scale stratigraphy is explained by the ratio of mixing rate to accumulation rate, which is much larger for the offshore mud deposit (27.34) than for the inner shelf mud deposit (1.65). these larger ratio allows biological mixing to destroy physical stratification.
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윤정수,박상운,Youn, Jeung-Su,Park, Sang-Woon 한국지구과학회 2000 한국지구과학회지 Vol.21 No.1
The purpose of this study is to elucidate the characteristic of this study is of attitudinal variation of water quality for nine representative springs in the Halla mountain region. The evolutional processes of the spring water also have been studied. Results of hydrogeochemical analyses show that Gwaneumsa spring is very high in pH. The spring waters from Yungsil, Namguksunwon, Sungpanark Oremok and Gwaneumsa which springs situated lower than 1000m in altitude are relatively high concentrations in chloride, sulphate, nitrate nitrogen and sodium ions, indicating that they are affected by surrounding pollution sources. The concentrations of bicarbonate, sulphate and hydrogen ions in spring waters increase when the precipitation increases, whereas the concentrations of nitrate nitrogen, chloride and calcium ions decrease with increasing amounts of precipitation. The magnesium, sodium and electrical conductivity are nearly independent of the precipitation. The spring waters in the Halla mountain region belong to the groups of sodium or potassium type and bicarbonate type, except the Baegrogdam and Wiseorm spring water. 본 연구는 한라산 지역에 분포하는 대표적인 9개 용천수에 대한 고도별 수질특성과 그 진화과정을 연구하였다. 조사 지역 9개 용천수의 수질분석결과 관음사용천수는 수소이온 농도에서 비정상적인 수질특성을 보였다. 해발고도 1000m 이하에 위치하는 영실, 남국선원, 성판악, 어리목 및 관음사용천수에서는 염소이온, 황산이온, 질산성질소 및 나트륨이온 함량이 높아 주변 육상오염원들에 의해 오염이 진행 중인 용천수로 분류된다. 중탄산이온, 황산이온 및 수소이온 농도는 강수량이 많았을 때 그 농도가 증가하였으며, 염소이온, 칼슘이온 및 질산성질소 농도는 강수량이 많았을 때 그 농도가 감소하였고, 마그네슘이온, 나트륨이온 및 전기비전도도 농도는 강수량의 영향이 미미하였다. 한라산 용천수는 백록담 담수와 윗세오름용천수를 제외한 전 용천수가 나트륨 또는 칼륨형(sodium or potassium type)과 중탄산형(bicarbonate type)의 용천수군으로 구분된다.
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제주해협 표층퇴적물의 특성 - 특히 점토광물을 중심으로 -
윤정수,강순석 한국지구과학회 1991 韓國地球科學會誌 Vol.12 No.3
The textural characteristics, the total suspended matter and the coarse fraction components of the surface sediments of the marine environment on the Cheju Strait are described and the distribution pattern of clay mineral discussed. The sediments are subdivied into ten textural classes; namely sand, slightly gravilly muddy sand, muddy sand, sandy clay, slightly gravelly sandy mud, mud and clay. the coarse sediments are distributed in the central and southeastern parts of the Cheju Strait which are bathymetric highs, whereas the fine-grained deposits are mainly distributed in the northeastern region, and the small scale of coarse and fine-grained mixed sediments are distributed in the western part of the study area. The high concentration of the total suspended matter in the study area gradually increase toward the northeastern nearshore area. The light minerals such as K-feldspar show a high content toward the northern region, which is related to the weathering of granites and metamorphic rooks on the adjacent lands, but the Na-Ca feldspars are relatively high near the northern part off Cheju Island. The illite is the most widespread clay mineral and the high concentrations of illite gradually increase toward the southern offshore. It is presumed that they are largely transported by the Kuroshio Current from the East China Sea such as Yellow Sea Warm Current and Tsushima Warm Current. Smectite is highly concentrated in the central part and arround off the Cheju Island it may have been partly derived from the central Yellow Sea by the local ocean current and the result of supplies of smectite altered from volcanic materials distributed in the Cheju Island. Therelative abundance of kaolinite shows a high in the northern nearshore area rather than in other regions, which are probably the results of supply from the southwestern Korea Rivers such as the Youngsan and Seomjin River. Chlorite shows partly similar distribution trend to that of kaolinite. This is related to the weathering of metamorphic rocks on adjacent lands. As to the controlling factors of the distribution pattern of clay minerals on the Cheju Strait, it is concluded that not only regional on-land geology but also local turbid plume and major ocean circulation are important.
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