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Let-It-Rain: A Web-based Stochastic Rainfall Generator Huidae Cho 1 Dekay Kim 2, Christian Onof 3, Minha Choi 4 April 20, 2016 1 Dewberry, Atlanta, GA 2 Hongik University, Seoul, Korea 3 Imperial College, London, UK 4 Sungkyunkwan University, Suwon, Korea
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Stochastic Rainfall Generator Generates synthetic rainfall time series based on the statistics of the past storm events Let-It-Rain: http://LetItRain.info Web-based using ArcGIS API for JavaScript Applications: General Use, Flood, Runoff Simulation period: January to December Unlimited number of simulations Click or enter coordinates Funded by the Ministry of Science, ICT and Future Planning, Korea For commercial use, contact Dekay Kim
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Stochastic Rainfall Generator (cont.) Uncertainty analysis of hydrologic phenomena such as flood, drought, etc. Fill data gap for water resources planning and design Climate change modeling http://www.brisbanetimes.com.au/content/dam/images/1/9/f/e/k/ image.gallery.galleryLandscape.600x400.1pmvn.png/1325987703890.jpg http://s4.firstpost.in/wp-content/uploads/2012/08/Drought_Boy_Afp.jpg
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Why Does It Matter? 1. Uncertainty Analysis
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Why Does It Matter? 1. Uncertainty Analysis (cont.) Curve Number Lag Time Prior knowledge about the model and study area Rainfall generator 100-year Floodplain Histogram of the Flooded Area Monte Carlo GLUE Statistical inference
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Why Does It Matter? 2. Filling Data Gap for Planning and Design Purposes Statistical generation of rainfall time series for ungaged locations 2554 + 143 NCDC rainfall gages
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Why Does It Matter? 3. Climate Change Modeling Future climate projections based on observed data Estimation of extreme weather events
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Modified Bartlett-Lewis Rectangular Pulse (MBLRP) Model λ [1/T] – Storm arrival rate, Poisson process β [1/T] – Rain cell arrival rate, Poisson process γ [1/T] – 1/Storm duration, Exponential distribution μ [L/T] – Rain cell intensity, Exponential distribution η [1/T] – 1/Rain cell duration, Exponential distribution ν [T], α [-] - Gamma distribution Normalized φ [-] = γ/η Normalized κ [-] = β/η Time [T] Intensity [L/T]
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Statistic Measures Four statistic measures Mean(Synthetic Rainfall) = Mean(Observed Rainfall) Variance(Synthetic Rainfall) = Variance(Observed Rainfall) Autocorrelation(Synthetic Rainfall) = Autocorrelation(Observed Rainfall) Probability of zero rainfall(Synthetic Rainfall) = Probability of zero rainfall(Observed Rainfall) Four accumulation levels: 1 hour, 3 hours, 12 hours, and 24 hours Total 4 x 4 = 16 statistic measures for each month
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Objective Function θ is the parameter vector (λ, ν, α, μ, φ, κ), n is the number of statistics being matched, F k is the k th statistic of the simulated rainfall time series, f k is the k th statistics of the observed rainfall time series, and w k is a weight factor given to the k th statistic. For runoff volume, higher w k for the mean For flood discharge, higher w k for the mean and variance For other simulations, equal weights
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Parameter Calibration Six-dimensional optimization problem Highly complicated surface of the objective function Highly multi-modal Gradient-based optimization methods cannot solve the problem Isolated-Speciation-based Particle Swarm Optimization (ISPSO) (Cho et al., 2011) was used Heuristic approach Derivative free Capable of finding not only global optimum but also local optima
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ISPSO in Action
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Calibrated Parameters
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Parameter Regionalization Estimated the MBLRP parameters at 2,697 NCDC rainfall gages across the United States Interpolated the parameters using the Ordinary Kriging technique Cross-validated the parameter maps (12 months x 6 parameters = 72 maps) at all the gages
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1 λ ν αμ φ κ
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Let-It-Rain Architecture ArcGIS Server MBLRP Parameter Maps Web Server MBLRP JavaScript Code 4. MBLRP Modeling Web Client 5. Parameters / Simulated Precipitation 1. Request 2. MBLRP Code 3. MBLRP Parameters
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Application to Urban Flood Modeling Flood Map of Simulated Rainfall and Design Rainfall (10 minute temporal resolution)
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Demonstration http://LetItRain.info http://LetItRain.info
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Conclusions Used the mean, variance, autocorrelation, and probability of zero rainfall for calibration of the MBLRP parameters Used the Ordinary Kriging technique for parameter regionalization Developed a web-based stochastic rainfall generator Application results show the validity of simulated rainfall events Future work includes inter-annual variability
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References Huidae Cho, Dongkyun Kim, Francisco Olivera, Seth D. Guikema, August 16, 2011. Enhanced Speciation in Particle Swarm Optimization for Multi-Modal Problems. European Journal of Operational Research 213 (1), 15-23. doi:10.1016/j.ejor.2011.02.026. doi:10.1016/j.ejor.2011.02.026 Dongkyun Kim, Francisco Olivera, Huidae Cho, Scott A. Socolofsky, June 2013. Regionalization of the Modified Bartlett-Lewis Rectangular Pulse Stochastic Rainfall Model. Terrestrial, Atmospheric and Oceanic Sciences 24 (3), 421- 436. doi:10.3319/TAO.2012.11.12.01(Hy).doi:10.3319/TAO.2012.11.12.01(Hy) Dongkyun Kim, Huidae Cho, Christian Onof, Minha Choi, March 2016. Let-It- Rain: A Web Application for Stochastic Point Rainfall Generation at Ungaged Basins and Its Applicability in Runoff and Flood Modeling. Stochastic Environmental Research and Risk Assessment. doi:10.1007/s00477-016-1234- 6.doi:10.1007/s00477-016-1234- 6
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