• 한국농공학회논문집
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• 제60권3호
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• pp.107-112
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• 2018

In this study, we conducted to analyze and quantify the amount of nitrogen supply into the rice paddies from the rainfall during cropping and non-crop periods. Rainfall monitoring conducted 85 times from June 2015 to December 2017. Nitrogen supply of cropping season ranged from 5.37 to 7.70 kg/ha, while non-cropping season were supplied from 3.97 to 4.42 kg/ha. The supply of T-N in the crop period was more than 60% of the total supply. And as a result of analyzing the correlation between the characteristics of rainfall and the supply amount, nitrogen concentrations in rainfall were decreased with increasing rainfall, but the supply amount was increased. Therefore, efforts should be made to increase the rainfall utilization and to increase the nitrogen supply of crops by increasing rainfall storage through drainage management.

• 한국농공학회논문집
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• 제58권5호
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• pp.91-99
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• 2016

High resolution rainfall data at 1-hour or a finer scale are essential for reliable flood analysis and forecasting; nevertheless, many observations, forecasts, and climate projections are still given at coarse temporal resolutions. This study aims to evaluate a chaotic method for disaggregation of 6-hour rainfall data sets so as to apply operational 6-hour rainfall forecasts of the Korean Meteorological Association to flood models. We computed parameters of a state-of-the-art multiplicative random cascade model with two combinations of cascades, namely uniform splitting and diversion, using rainfall observations at Seoul station, and compared statistical performance. We additionally disaggregated 6-hour rainfall time series at 58 stations with the uniform splitting and evaluated temporal transferability of the parameters and changes in multifractal properties. Results showed that the uniform splitting outperformed the diversion in reproduction of observed statistics, and hence is better to be used for disaggregation of 6-hour rainfall forecasts. We also found that multifractal properties of rainfall observations has adequate temporal consistency with an indication of gradually increasing rainfall intensity across South Korea.

• 한국물환경학회지
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• 제30권6호
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• pp.622-631
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• 2014

The purpose of this research was to find a proper disposal rainfall extent to improve water quality. SWMM was applied to select catchment area and tested first flush load and rainfall extent. BOD 40mg/L was selected to dispose the first flush and sewer overflow with the same as the criteria of Sewerage Act. Design rainfall, BOD load ratio of first flush sewer overflow, and the ratio of disposal flow were analyzed under various rainfall distribution. BOD load and design rainfall to treat overflow in situation of first flush extent with 4.3~17.4% were 56~87% and 3.8~6.8 mm/day, respectively. In urban area, first flush loads were not correspond to land activities, but tend to increase with increasing rainfall amount and drainage area. The more the distribution of rainfall is similar to Huff-frontal or central distribution of rainfall, the more increase the first flush loads.

• 한국방재학회 논문집
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• 제1권1호
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• pp.103-115
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• 2001

현재 소규모 유역에서의 수공구조물의 설계시 확률강우강도식을 사용하여 강우량을 산정하는 것이 일반적인 적용방법으로 이용되어지고있다. 확률강우의 산정은 그 자체로서 불확실성을 많이 내포하고 있으나 현실적으로 강우의 비선형성을 해석함에 있어 단순화는 배제 할 수 없는 필요사항이다. 따라서 본 연구에서는 확률강우량 산정을 위한 강우강도식의 산정에 있어서 그 비선형성을 잘 모의할 수 있는 방법에 관하여 연구하여 보았다. 연구결과에 의하면 유전자 알고리즘이 시산법이나 비선형계획법의 일종인 Powell 기법에 비하여 더 신뢰성 높은 방법임을 알 수 있었다.

• 한국농공학회지
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• 제38권2호
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• pp.108-122
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• 1996

This study was to introduced estimation model for optimum probabilistic rainfall intensity on hydrological area. Originally, probabilistic rainfall intensity formula have been characterized different coefficient of formula and model following watersheds. But recently in korea rainfall intensity formula does not use unionize applyment standard between administration and district. And mingle use planning formula with not assumption model. Following the number of year hydrological duration adjust areal index. But, with adjusting formula applyment was without systematic conduct. This study perceive the point as following : 1) Use method of excess probability of Iwai to calculate survey rainfall intensity value. 2) And, use method of least squares to calculate areal coefficient for a unit of 157 rain gauge station. And, use areal coefficient was introduced new probabilistic rainfall intensity formula for each rain gauge station. 3) And, use new probabilistic rainfall intensity formula to adjust a unit of fourteen duration-a unit of fifteen year probabilistic rainfall intensity. 4) The above survey value compared with adjustment value. And use three theory of error(absolute mean error, squares mean error, relative error ratio) to choice optimum probabilistic rainfall intensity formula for a unit of 157 rain gauge station.

• 한국수자원학회논문집
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• 제32권3호
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• pp.247-254
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• 1999

우리 나라 주요 우량관측소 22개 지점의 매년 최대치 강우자료에 대하여 빈도해석을 실시하였다. 매개변수 추정방법은 모멘트법, 확률가중 모멘트법, 최우도법 등이며, 매개변수 적합성, 도시적 해석, 분리효과, 적합도 검정결과 GEV 분포가 우리 나라 강우자료에 대하여 가장 적합한 확률분포형으로 나타났다. 선정된 GEV 분포형을 모집단의 확률분포형으로 가정하여 재현기간별 확률강우량을 산정하므로써 지역적 해석을 실시하였으며, 정확도 있는 선형화 기법을 통해 회귀분석을 실시하여 확률강두강도식을 유도하였다. 본 연구에서 유도된 확률강우강도식은 실무차원에서 임의 지속기간의 재현기간별 확률강우량을 간편하게 구할 수 있을 것으로 판단된다.

• 물과 미래
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• 제14권3호
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• pp.47-54
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• 1981

우리나라의 주요 도시 서울, 부산, 대구, 광주의 지점강우량에 대하여 확률적인 방법과 M년 최대치법에 의하여 그 특성이 해석되었으며 일본의 해석결과와도 비교되었다. 본 연구에서 얻어진 결과는 다음과 같다. T년확률강우가 N년 동안에 발생하지 않은 확률은 관측치로부터 분석된 값과 비교하여 볼 때 이론치보다 작았으며 일본의 결과보다는 컸다. M년 10분 최대치가 N년 동안에 발생하지 않은 확률의 평균치는 이론치보다 컸으며 M년 1시간 최대치는 이론치보다 작았고 M년 1일 최대치는 이론치와 거의 일치했으며 일본의 경우는 이론치보다 작았다. 상기 결과에 의하여 확률적인 면에서 본다면 M년 최대강우를 설계량으로 택하는 것이 T년 확률강우보다 안전측이라고 생각된다.

• 한국환경과학회지
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• 제24권4호
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• pp.383-391
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• 2015

As occurrence of gradually increasing extreme temperature events in Jeju Island, a hybrid downscaling technique that simultaneously applies by dynamical method and statistical method has implemented on design rainfall in order to reduce flood damages from severe storms and typhoons.As a result of computation, Case 1 shows a strong tendency to excessively compute rainfall, which is continuously increasing. While Case 2 showed similar trend as Case 1, low design rainfall has computed by rainfall in A1B scenario. Based on the design rainfall computation method mainly used in Preventive Disaster System through Pre-disaster Effect Examination System and Basic Plan for River of Jeju Island which are considering climatic change for selecting 50-year and 100-year frequencies. Case 3 selecting for Jeju rain gage station and Case 1 for Seogwipo rain gage station. The results were different for each rain gage station because of difference in rainfall characteristics according to recent climatic change, and the risk of currently known design rainfall can be increased in near future.

• Water Engineering Research
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• 제2권1호
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• pp.63-72
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• 2001

The variation of sampling errors was characterized using the Waymire-Gupta-Rodriguez-Iturbe multi-dimensional rainfall model(WGR model). The parameters used for this study are those derived by Jung et al. (2000) for the Han River Basin using a genetic algorithm technique. The sampling error problems considered are those for using raingauge network, satellite observation and also for both combined. The characterization of sampling errors was done for each month and also for the downstream plain area and the upstream mountain area, separately. As results of the study we conclude: (1) The pattern of sampling errors estimated are obviously different from the seasonal pattern of monthly rainfall amounts. This result may be understood from the fact that the sampling error is estimated not simply by considering the rainfall amounts, but by considering all the mechanisms controlling the rainfall propagation along with its generation and decay. As the major mechanism of moisture source to the Korean Peninsula is obviously different each month, it seems rather normal to provide different pattern of sampling errors from that of monthly rainfall amounts. (2) The sampling errors estimated for the upstream mountain area is about twice higher than those for the down stream plain area. It is believed to be because of the higher variability of rainfall in the upstream mountain arean than in the down stream plain area.

• 한국수자원학회논문집
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• 제36권2호
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• pp.237-249
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• 2003

우량계에 대한 바람의 영향은 우량의 감소와 강우자료의 일관성에 영향을 미치게 된다. 이러한 강우량을 보정하기 위해서는 강우의 감소율을 산정 할 수 있는 연구가 필요하다. 이러한, 강우의 감소에 대한 연구는 거의 수행되지 않았으며, 적절한 보정기법에 대한 연구는 미흡한 실정이다. 본 연구에서는 강우의 입자 크기에 따른 낙하속도를 산정 하였다. 이를 이용하여 강우의 입자크기에 따라 강우의 감소율을 보정할 수 있는 모형을 실험을 통하여 검토하였다. 실험결과 강우의 감소율은 강우의 강도와는 상관없고 강우의 입자크기에 따라 영향을 받는 것으로 나타났다. 본 연구에서 산정된 강우감소율은 실험결과와 잘 일치하고 있으며, 보정계수로 사용가능 한 것으로 판단된다.