Paper No. JAWRA-12-0060-P of the Journal of the American Water Resources Association (JAWRA).Discussions are open until six months from print publication.
The Impact of Asynchronicity on Event-Flow Estimation in Basin-Scale Hydrologic Model Calibration1
Article first published online: 10 DEC 2012
© 2012 American Water Resources Association
JAWRA Journal of the American Water Resources Association
Volume 49, Issue 2, pages 300–318, April 2013
How to Cite
Joseph, J. F., Sharif, H. O., Arnold, J. G. and Bosch, D. D. (2013), The Impact of Asynchronicity on Event-Flow Estimation in Basin-Scale Hydrologic Model Calibration. JAWRA Journal of the American Water Resources Association, 49: 300–318. doi: 10.1111/jawr.12011
- Issue published online: 1 APR 2013
- Article first published online: 10 DEC 2012
- Received March 8, 2012; accepted October 16, 2012.
- surface water hydrology;
- nonlinear dynamics;
- uncertainty analysis;
- computational methods
Abstract: The calibration of basin-scale hydrologic models consists of adjusting parameters such that simulated values closely match observed values. However, due to inevitable inaccuracies in models and model inputs, simulated response hydrographs for multiyear calibrations will not be perfectly synchronized with observed response hydrographs at the daily time step. An analytically derived formula suggests that when timing errors are significant, traditional calibration approaches may generally underestimate the total event-flow volume. An event-adaptive time series is developed and incorporated into the Nash-Sutcliffe Efficiency objective function to diagnose the potential impact of event-flow synchronization errors. Test sites are the 50 km2 Subwatershed I of the Little River Experimental Watershed (LREWswI) in southeastern Georgia, and the 610 km2 Little Washita River Experimental Watershed (LWREW) in southwestern Oklahoma, with the Soil and Water Assessment Tool used as the hydrologic model. Results suggest that simulated surface runoff generation is 55% less for LREWswI when the daily time series is used compared with when the event-adaptive technique is used. Event-flow generation may also be underestimated for LWREW, but to a lesser extent than it may be for LREWswI, due to a larger portion of the event flow being lateral flow.