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311
Locally Enriched Quadtree Grid Numerical Model for Nearshore Circulation in the surf zone
Locally Enriched Quadtree Grid Numerical Model for Nearshore Circulation in the surf zone
Koo-Yong Park | 한국 수자원학회 | 2000
להדפיס
312
Determination of Trophic State and Phosphorus Model in the Ki Heung Reservoir
Determination of Trophic State and Phosphorus Model in the Ki Heung Reservoir
Do-Hun Lee | 한국 수자원학회 | 2000
להדפיס
313
Characterization of Pool-riffle Sequences in Solute Transport Modeling of Streams
Characterization of Pool-riffle Sequences in Solute Transport Modeling of Streams
Il-Won Seo | 한국 수자원학회 | 2000
להדפיס
314
Modeling of Critical Flux Conditions in Crossflow Microfiltration
Modeling of Critical Flux Conditions in Crossflow Microfiltration
Suhan Kim | 한국 수자원학회 | 2000
להדפיס
315
Forecasting Water Levels of Bocheong River Using Neural Network Model
Forecasting Water Levels of Bocheong River Using Neural Network Model
Jitae Kim | 한국 수자원학회 | 2000
להדפיס
316
Development of a Windows-based Predictive Model for Estimating Sediment Resuspension and Contaminant Release form Dredging Operations
Development of a Windows-based Predictive Model for Estimating Sediment Resuspension and Contaminant Release form Dredging Operations
Chung-Hwan Je | 한국 수자원학회 | 2000
להדפיס
317
Characterization of Rainrate Fields Using a Multi-Dimensional Precipitation Model
Characterization of Rainrate Fields Using a Multi-Dimensional Precipitation Model
Chulsang Yoo | 한국 수자원학회 | 2000
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318
Characterization Study for the Coupled Atmosphere, streamflow Modeling in Korea
Characterization Study for the Coupled Atmosphere, streamflow Modeling in Korea
Jae-Young Park | 한국 수자원학회 | 2000
להדפיס
319
Caution on Regional Flood Frequency Analysis Based on Weibull Model
Caution on Regional Flood Frequency Analysis Based on Weibull Model
Jun-Haeng Heo | 한국 수자원학회 | 2000
להדפיס
320
A Preliminary Study for the Coupled Atmosphere-Streamfiow Modeling in Korea
A Preliminary Study for the Coupled Atmosphere-Streamfiow Modeling in Korea
Deg-Hyo Bae | 한국 수자원학회 | 2000
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