Assessment of a hydrologic model's reliability in simulating flow regime alterations in a changing climate

• Published in: Hydrological processes Vol. 30; no. 15; pp. 2628 - 2643
• Main Authors: Shrestha, Rajesh R., Schnorbus, Markus A., Peters, Daniel L.
• Format: Journal Article
• Language: English
• Published: Chichester Blackwell Publishing Ltd 15.07.2016; Wiley Subscription Services, Inc
• Subjects: Alterations; Basins; Climate; Climate models; Computer simulation; Copyright; Direction; El Nino; El Nino phenomena; El Nino-Southern Oscillation event; ENSO; Freshwater; Hydrologic models; Hydrologic processes; Hydrologic regime; Hydrology; Hydrology models; Indicators; indicators of hydrologic alteration; Infiltration; Infiltration capacity; Marine; model evaluation; Pacific Decadal Oscillation; Pacific Northwest; PDO; Reliability; Reliability analysis; Replication; River basins; Southern Oscillation; Stream discharge; Stream flow; Streamflow changes; Teleconnections; Watersheds; Canada; Canada, British Columbia, Fraser R. basin; ANW, Canada; I, Pacific
• ISSN: 0885-6087; 1099-1085
• DOI: 10.1002/hyp.10812

It is a common practice to employ hydrologic models for assessing present and future states of watersheds and assess the degree of alterations for a range of hydrologic indicators. Previous studies indicate that the hydrologic model may not be able to replicate some of the indicators of interest, which raises questions on the reliability of model simulated changes. Hence, we initiated a study to evaluate the replicability of the streamflow changes by employing the widely used variable infiltration capacity hydrologic model for sub‐basins and mainstem of the Fraser River Basin, Canada. Given that the hydrologic regime of the region is known to be influenced by teleconnections to the Pacific Decadal Oscillation (PDO) and El Niño–Southern Oscillation (ENSO), we used hydrologic responses to the PDO and ENSO states as analogues for evaluating the model's ability to simulate climate‐induced changes. The results revealed that the qualitative patterns of response, such as lower flows for the warm PDO state compared to the cool state, and progressively higher flows for the warm, neutral and cool ENSO states, were generally well reproduced for most hydrologic indicators. Additionally, while the directions of change between the different PDO and ENSO states were mostly well replicated, the magnitude of change for some of the indicators showed considerable differences. Hence, replicability of both magnitude and direction of change need to be carefully examined before using the simulated indicators for assessing future hydrologic changes, and a reliable replication increases the confidence of projected changes. Copyright © 2016 Her Majesty the Queen in Right of Canada. Hydrological Processes. © 2016 John Wiley & Sons, Ltd.