A Comparative Evaluation of Using Rain Gauge and NEXRAD Radar-Estimated Rainfall Data for Simulating Streamflow

被引:5
|
作者
Ahmed, Syed Imran [1 ,2 ]
Rudra, Ramesh [1 ]
Goel, Pradeep [3 ]
Khan, Alamgir [4 ]
Gharabaghi, Bahram [1 ]
Sharma, Rohit [5 ]
机构
[1] Univ Guelph, Sch Engn, Water Resources Engn, Guelph, ON N1G 2W1, Canada
[2] NED Univ Sci & Technol, Dept Civil Engn & Technol, Karachi 75270, Pakistan
[3] Minist Environm Conservat & Pk, Etobicoke, ON M9P 3V6, Canada
[4] Univ Agr, MNS Dept Agr, Multan 60000, Pakistan
[5] Alberta Energy Regulator AER, Water Engn, Calgary, AB T2P 0R4, Canada
关键词
rain gauge; radar; rainfall; hydrologic model; runoff; streamflow; WEATHER RADAR; FLOOD PREDICTION; RIVER-BASIN; MODEL; PRECIPITATION; ACCURACY; CLASSIFICATION; WATER; UNCERTAINTY; SENSITIVITY;
D O I
10.3390/hydrology9080133
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Ascertaining the spatiotemporal accuracy of precipitation is a challenge for hydrologists and planners for flood protection measures. The objective of this study was to compare streamflow simulations using rain gauge and radar data from a watershed in Southern Ontario, Canada, using the Hydrologic Engineering Center's event-based distributed Hydrologic Modeling System (HEC-HMS). The model was run using the curve number (CN) and the Green and Ampt infiltration methods. The results show that the streamflow simulated with rain gauge data compared better with the observed streamflow than the streamflow simulated using radar data. However, when the Mean Field Bias (MFB) corrections were applied, the quality of the streamflow results obtained from radar rainfall data improved. The results showed no significant difference between the simulated streamflow using the SCS and the Green and Ampt infiltration approach. However, the SCS method is reasonably more appropriate for modeling the runoff at the sub-basin-scale than the Green and Ampt infiltration approach. With the SCS method, the simulated and observed runoff amount obtained using rain gauge rainfall showed an R-2 value of 0.88 and 0.78 for MFB-corrected radar and 0.75 for radar only. For the Green and Ampt modeling option, the R-2 value for the simulated and observed runoff amounts were 0.87 with rain gauge, 0.66 with radar only, and 0.68 with MFB-corrected radar rainfall inputs. The NSE values for rain gauge input ranged from 0.65 to 0.35. Overall, three values were less than 0.5 for streamflow for both the methods. For seven radar rainfall events, the NSE was greater than 0.5, with a range of very good to satisfactory. The analysis of RSR showed a very good comparison of stream flow using the SCS curve number method and Green and Ampt method using different rainfall inputs. Only one value, the 2 November 2003 event, was above 0.7 for rain gauge-based streamflow. The other RSR values were in the range of "very good". Overall, the study showed better results for the simulated runoff with the MFB-corrected radar rainfall when compared with the simulations obtained using radar rainfall only. Therefore, MFB-corrected radar could be explored as a substitute rainfall source.
引用
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页数:36
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