• 한국환경과학회지
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• 제13권7호
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• pp.637-643
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• 2004

A new method of automatic recording raingauge is developed to measure rainfall with 0.01mm resolution. This use two different signals to measure rainfall more accurately compare than other raingauges. One is weight of the tipping bucket with rainfall amount and the other is pulse from tipping bucket reverse. New method applied 1 mm tipping bucket mechanism and install loadcell under tipping bucket mechanism for measuring rainfall weight. Loadcell measure weight of rainfall until 1 mm with 0.01 mm resolution and more than 1 mm than bucket reverse and pulse signal generate, after that loadcell measure weight again. The validation of new instrument was examined in the room 65 mm/hour rainfall rate total 53 mm range. There is below than 1 % error of absolute rainfall amount and 0.01 mm resolution. The field test of instrument was carried out by comparing its measured values with values recorded by weight type and standard type on June 1 2003 at Terrestrial Environmental Research Center at Tsukuba University in Tsukuba of Japan, when it has recorded total amount of 40.58 mm rainfall by standard raingauge and new raingauge recorded 41.032 mm. Same rainfall intensity pattern observed in field observation with weight type raingauge. Rainfall intensity between weight type and Lee-A type raingauge reached 0.9947 correlation in 3 minute average.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2007년도 학술발표회 논문집
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• pp.178-182
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• 2007

In this study, we evaluated current raingauge network of Soyanggang dam region applying spatial-correlation analysis and Entropy theory to recommend an optimized raingauge network. In the process of analysis, correlation distance of raingauge stations is estimated and evaluated via spatial-correlation method and entropy method. From this correlation distances, respective influencing radii of each dataset and each methods is assessed. The result of correlation and entropy analysis has estimated correlation distance of 25.546km and influence radius of 7.206km, deducing a decrease of network density from $224.53km^2$ to $122.47km^2$ which satisfy the recommended minimum densities of $250km^2$ in mountainous regions(WMO, 1994) and an increase of basin coverage from 59.3% to 86.8%. As for the elevation analysis the relative evaluation ratio increased from 0.59(current) to 0.92(optimized) resulting an obvious improvement.

• 한국수자원학회:학술대회논문집
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• 한국수자원학회 2003년도 학술발표회논문집(1)
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• pp.93-100
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• 2003

In order to use radar rainfall data for flood management, it is necessary to study and develop a method for optimum error correction to obtain radar rainfall values that agree closely with surface rainfall data. This paper proposes an optimum estimation method for calculating rainfall in a river basin by using data from surface raingauges and radar raingauge systems. This paper also reports on recent applications of radar raingauge systems for accurate simulation of flood discharge based on river basin rainfall values obtained from radar raingauge systems.

• 대기
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• 제27권2호
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• pp.251-258
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• 2017

The standard weighing raingauges have a capacity limit in measuring the amounts of precipitation. Exceptions are those using a siphon to drain the collected water during observations. To reduce the drain time of the siphon type or to overcome the hassles associated with the manual emptying of the bucket for measuring, the most of weighing gauges use a large bucket for storing of rainwater to be measured. To avoid the above-mentioned adverse requirements, we propose a paired barrel for a weighing raingauge. The paired barrel may improve the accuracy of the weighing raingauges by getting rid of their capacity limit and make the gauges smaller in size and lighter in weight than the conventional ones. We showed its proper function and the feasibility of realization by testing a prototype paired barrel.

• 한국환경과학회지
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• 제11권10호
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• pp.1055-1060
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• 2002

A new method of automatic recording raingauge is developed to measure rainfall 1200mm full scale with high accuracy and resolution. The principle of new instrument is to detect a weight change of a buoyant weight according to a change in water level of raingauge measured by the use of a strain gauge load cell. This method has the advantage of increasing measurement accuracy, since no moving equipment is used. Laboratory test of the instrument was recorded 0.4% error of 190mm rainfall amount. The validity of new instrument was examined by comparing its measured values with values recorded by automatic weather station on June 24 to 25 2001 at Daegu Meteorological Station, when there is 148.3mm rainfall amount. In spite of much rainfall there is only 0.77mm difference of total rainfall amount. This instrument was accomplished high accuracy and resolution at field test in much rainy day.

• 한국지반공학회:학술대회논문집
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• 한국지반공학회 2000년도 가을 학술발표회 논문집
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• pp.607-614
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• 2000

A cost-effective automated slope monitoring system is developed to monitor hazardous cut slopes along highways. This automated slope monitoring system consists of data-collection and visual monitoring, data-transmitting, database and internet service, and alarm system. Wire-line extensometer, automatic raingauge, and CCD camera are selected as monitoring instruments in this system, after consideration of failure characteristics of roadside cut slopes in the country. This paper describes the important features of this newly developed automated slope monitoring system.

• 한국습지학회지
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• 제16권1호
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• pp.103-112
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• 2014

면적평균강우량의 산정은 가용 수자원의 정확한 양을 파악하고 강우-유출해석에 필수적인 입력자료이기 때문에 매우 중요하다. 이와 같은 면적평균강우량의 정확한 산정을 위한 필수적인 조건은 강우관측망의 균일한 공간적 분포이다. 본 연구에서는 보다 향상된 유역 면적평균강우량 산정을 위한 강우관측망의 공간분포 평가방법론을 제시하고, 이를 한강 및 금강 유역에 적용하였다. 강우관측소의 공간적 분포 특성은 최근린 지수(nearest neighbor index)를 이용하여 정량화하였다. 유역별 강우관측소의 공간적 분포가 면적평균강우량 산정에 미치는 영향을 평가하기 위하여 2013년의 강우사상에 대해 산술평균법, 티센가중법, 추정이론을 이용하여 면적평균강우량을 산정하고 각 경우에 대해 추정오차를 평가하였다. 그 결과 공간분포가 우수한 유역은 면적평균강우량의 추정오차가 상대적으로 작으며, 반대로 공간분포가 왜곡된 유역의 경우는 상대적으로 추정오차가 큼을 확인하였다.

• 한국수자원학회논문집
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• 제36권2호
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• pp.173-181
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• 2003

본 연구에서는 강우가 공간적으로 균질하며 아울러 그 공간상관구조도 지수함수를 따른다고 가정하여 남한강 유역의 강우관측망을 평가하였고 아울러 WMO의 기준과 비교하였다. 그 결과를 정리하면 다음과 같다. (1) 남한강유역은 WMO의 기준으로 볼 때 산지도 평지도 아닌 중간적 특성을 나타낸다. 그러나 남한강 상류부에서 관측된강우의 공간상관거리는 남한강 하류부에서 관측된 강우의 공간상관거리에 비해 짧게 나타나며 따라서 상류부와 하류부는 그 강우특성이 구별된다. (2) 남한강 유역의 강우관측망을 평가하는 기준은 대략 상위 50% 정도를 대표하는 상관거리 수준이 되어야 할 것으로 보이며 이 경우 적절한 우량계 사이의 거리는 상류부와 하류부 각각 18.2km와 21.1km로 추정된다. 단순히 강우계의 밀도를 평가할 때 남한강의 경우는 WMO의 산지기준을 초과하는 수준이다. (3) 남한강 유역의 우량계 분포를 검토한 결과, 특히 WMO의 온대지역 산지기준을 적용한 결과 우랑계의 공간분포가 적절하지 않음을 파악할 수 있었다. 그러나 본 연구에서 제안하는 상위 50% 정도를 대표하는 상관거리를 이용하는 경우에는 대략 5 - 6 지점 정도의 우량계 신설이 필요한 것으로 나타났다.

• 물과 미래
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• 제48권9호
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• pp.36-49
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• 2015

• 한국농림기상학회:학술대회논문집
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• 한국농림기상학회 2016년도 추계 학술발표논문집
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• pp.91-93
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• 2016