• Atmosphere
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• v.22 no.3
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• pp.357-365
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• 2012

High spatio-temporal resolution hydrologic components can give important information to monitor natural disaster. The objective of this study is to create high spatial-temporal resolution gridded hydrologic components using TOPLATS distributed land surface model and evaluate their accuracy. For this, Andong dam basin is selected as study area and TOPLATS model is constructed to create hourly simulated values in every $1{\times}1km^2$ cell size. The observed inflow at Andong dam and soil moisture at Andong AWS site are collected to directly evaluate the simulated one. RMSEs of monthly simulated flow for calibration (2003~2006) and verification (2007~2009) periods show 36.87 mm and 32.41 mm, respectively. The hourly simulated soil moisture in the cell located Andong observation site for 2009 is well fitted with observed one at -50 cm. From this results, the cell based hydrologic components using TOPLATS distributed land surface model show to reasonably represent the real hydrologic condition in the field. Therefore the model driven hydrologic information can be used to analyze local water balance and monitor natural disaster caused by the severe weather.

• Journal of Korea Water Resources Association
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• v.49 no.1
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• pp.19-28
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• 2016

The objective of this study is the generation of the gridded flash flood index using the gridded hydrologic components of TOPLATS land surface model and statistic flash flood index model. The accuracy of this method is also examined in this study. The study area is the national capital region of Korea, and 38 flash flood damages had occurred from 2009 to 2012. The spatio-temporal resolutions of land surface model are 1 h and 1 km, respectively. The gridded meteorological data are generated using the inverse distance weight method with automatic weather stations (AWSs) of Korea Meteorological Administration (KMA). The hydrological components (e.g., surface runoff, soil water contents, and water table depth) of cells corresponding to the positions of 38 flood damages reasonably respond to the cell based hourly rainfalls. Under the total rainfall condition, the gridded flash flood index shows 71% to 87% from 4 h to 6 h in the lead time based on the rescue request time and 42% to 52% of accuracy at 0 h which means that the time period of the lead time is in a limited rescue request time. From these results, it is known that the gridded flash flood index using the cell based hydrological components from land surface model and the statistic flash flood index model have a capability to predict flash flood in the mountainous area.

• Proceedings of the Korea Water Resources Association Conference
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• 2015.05a
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• pp.525-525
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• 2015

국립기상과학원은 국가 물관리를 효율적으로 지원하기 위하여 TOPLATS(TOPmodel based Land-Atmosphere Transfer Scheme) 지면모델 기반을 활용한 전국 수문기상 분석 및 예측정보 생산체계를 구축하였다. TOPLATS 지면모델에서는 토양, 식생 등을 표현하기 위한 다양한 매개변수들이 사용되고 있으며, 그 중에서도 토양 속성과 관련 매개변수들은 토양수분, 증발산 등의 수문기상요소 생산에 큰 영향을 미치고 있어 현실적인 토양 특성에 대한 고려가 요구된다. 본 연구는 국립농업과학원의 토양도 정보를 이용하여 TOPLATS 지면모델에서 요구되는 토양 속성 및 관련 매개변수를 산정하고 이를 모델에 적용하고자 하였다. TOPLATS 모델에 사용되는 토양 매개변수는 총 22개 이며, 본 연구에서는 국립농업과학원에서 제공한 총 405개의 토양통에 대한 매개변수를 각각 산정하였다. TOPLATS 모델을 강제하기 위한 기상자료는 동네예보 분석자료, KLAPS(Korea Local Analysis and Prediction System) 분석자료, 입사 단 장파 복사량은 ASOS 관측자료를 기반으로 한 5km 해상도의 남한 격자자료이며, 2010~2013년 기간의 토양수분, 증발산량에 대한 검증 연구를 수행하였다. 본 연구의 결과는 기존의 11개 토양속성정보로 산출된 결과와 비교 분석하여 추후 제시할 예정이며, 본 연구에서 산출된 국내 토양 특성을 반영한 고해상도 수문기상정보는 향후 홍수 예측 및 가뭄 평가에 활용 할 수 있을 것으로 기대된다.

• Proceedings of the Korea Water Resources Association Conference
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• 2015.05a
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• pp.7-7
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• 2015

가뭄 및 홍수 등 재해를 방지하고 효율적인 물 관리를 위해서는 지표와 대기 사이에 이루어지는 수문기상 요소의 정량화가 필요하다. 수문기상요소는 관측을 통해 파악하는 것이 가장 정확하지만 광범위한 지역에 대한 관측은 한계가 있으므로 일반적으로 지면모델(Land Surface Model)을 많이 이용한다. 본 연구에서 Noah LSM(Noah Land Surface Model)과 TOPLATS(TOPmodel based Land-Atmosphere Transfer Scheme) 및 DHSVM(Distributed Hydrology Soil Vegetation Model)의 세 모델을 활용하여 안동댐 유역의 수문기상정보를 산출하고 관측자료와 검증함으로 각 모델의 특성을 분석하자 한다. 본 연구에서 사용된 관측자료는 국립기상과학원에서 운영중인 안동댐 유역 플럭스타워의(A6, A7) 지표근처 기상장과 에너지 요소이다. '13년 10월부터 '14년 11월까지 기간에 대해 각 지점에서 관측된 현열 및 잠열 플럭스의 품질관리를 수행하였으며, 이 자료를 본 연구의 검증자료로 활용하였다. 각 모델을 강제하기 위한 지표근처 기상자료는 두 지점에서 관측된 기온, 풍향 풍속, 상대습도, 강수, 지중온도 및 장 단파 복사량이며, 각 모델에서 산출된 잠열 및 현열 플럭스, 토양수분과 증발산량을 관측값과 비교 검증하였다. 본 연구결과는 한국수자원학회 학술발표회를 통하여 소개될 예정이며, 향후 멀티모델 앙상블 시스템 구축에 기초자료로 활용될 것으로 기대된다.

• Journal of Digital Convergence
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• v.15 no.11
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• pp.245-250
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• 2017

Flash floods is defined as the flooding of intense rainfall over a relatively small area that flows through river and valley rapidly in short time with no advance warning. So that it can cause damage property and casuality. This study is to establish the flash-flood warning system using 38 accident data, reported from the National Disaster Information Center and Land Surface Model(TOPLATS) between 2009 and 2012. Three variables were used in the Land Surface Model: precipitation, soil moisture, and surface runoff. The three variables of 6 hours preceding flash flood were reduced to 3 factors through factor analysis. Decision tree, random forest, Naive Bayes, Support Vector Machine, and logistic regression model are considered as big data methods. The prediction performance was evaluated by comparison of Accuracy, Kappa, TP Rate, FP Rate and F-Measure. The best method was suggested based on reproducibility evaluation at the each points of flash flood occurrence and predicted count versus actual count using 4 years data.

• Journal of Korea Water Resources Association
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• v.47 no.1
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• pp.25-35
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• 2014

The objective of this study is to evaluate TOPLATS land surface model performance through comparison of results of water and energy balance analysis. The study area is selected Nakdong river basin and high resolution hydrometeorological components of which spatio-temporal resolution is 1 hr and 1 km are simulated during 2003 to 2013. The simulated daily and monthly depth of flows are well fitted with the observed one on Andong and Hapcheon dam basin. In results of diurnally analysis of energy components, change pattern throughout the day of net radiation, latent heat, sensible heat, and ground heat under energy balance analysis have higher accuracy than ones under water balance analysis at C3 and C4 sites. Especially, root mean square errors of net radiation and latent heat at C4 site are shown very low as 22.18 $W/m^2$ and 7.27 $W/m^2$, respectively. Mean soil moisture and evapotranspiration in summer and winter are simulated as 36.80%, 33.08% and 222.40 mm, 59.95 mm, respectively. From this result, when we need high resolution hydrometeorological components, energy balance analysis is more reasonable than water balance analysis. And this results will be used for monitor and forecast of weather disaster like flood and draught using spatial hydrometeorological information.