H21I-1508
Regional statistical assessment of WRF-Hydro and IFC Model stream Flow uncertainties over the State of Iowa

Tuesday, 15 December 2015
Poster Hall (Moscone South)
Mohamed ElSaadani1, Felipe Quintero2, Radoslaw Goska2, Witold F Krajewski1, Tim Lahmers3, Scott Small2 and David J Gochis4, (1)University of Iowa, Iowa City, IA, United States, (2)IIHR—Hydroscience and Engineering, Iowa City, IA, United States, (3)University of Arizona, Tucson, AZ, United States, (4)National Center for Atmospheric Research, Boulder, CO, United States
Abstract:
This study examines the performance of different Hydrologic models in estimating peak flows over the state of Iowa. In this study I will compare the output of the Iowa Flood Center (IFC) hydrologic model and WRF-Hydro (NFIE configuration) to the observed flows at the USGS stream gauges. During the National Flood Interoperability Experiment I explored the performance of WRF-Hydro over the state of Iowa using different rainfall products and the resulting hydrographs showed a “flashy” behavior of the model output due to lack of calibration and bad initial flows due to short model spin period. I would like to expand this study by including a second well established hydrologic model and include more rain gauge vs. radar rainfall direct comparisons. The IFC model is expected to outperform WRF-Hydro’s out of the box results, however, I will test different calibration options for both the Noah-MP land surface model and RAPID, which is the routing component of the NFIE-Hydro configuration, to see if this will improve the model results. This study will explore the statistical structure of model output uncertainties across scales (as a function of drainage areas and/or stream orders). I will also evaluate the performance of different radar-based Quantitative Precipitation Estimation (QPE) products (e.g. Stage IV, MRMS and IFC’s NEXRAD based radar rainfall product. Different basins will be evaluated in this study and they will be selected based on size, amount of rainfall received over the basin area and location. Basin location will be an important factor in this study due to our prior knowledge of the performance of different NEXRAD radars that cover the region, this will help observe the effect of rainfall biases on stream flows. Another possible addition to this study is to apply controlled spatial error fields to rainfall inputs and observer the propagation of these errors through the stream network.