Technical Papers
Jun 8, 2013

Gauging the Ungauged Basin: Relative Value of Soft and Hard Data

Publication: Journal of Hydrologic Engineering
Volume 20, Issue 1

Abstract

The long-standing issue of hydrological predictions in ungauged basins has received increased attention due to the recent International Association of Hydrological Sciences (IAHS) decade on predictions in ungauged basins (PUB). Since the outset of PUB, many have noted that the best way to confront an ungauged basin is to first make some basic streamflow measurements. This study explores the value of a rudimentary gauging campaign for making predictions in an ungauged basin. The well-studied Maimai watershed in New Zealand was used as a hypothetical ungauged basin, and this study was designed to start with no runoff data and add iteratively different subsets of the available data to constrain the calibration of a simple three-reservoir conceptual catchment model. These subsets included single runoff events or a limited number of point values—in other words, what could be measured with limited, campaign-like field efforts in an ungauged basin. In addition, different types of soft data were explored to constrain the model calibration. Model simulations were validated using the available runoff data from different years. It was found that surprisingly little runoff data were necessary to derive model parameterizations that provided good results for the validation periods, especially when these runoff data were combined with soft data. The relative value of soft data increased with decreasing amount of streamflow data. The findings from the Maimai watershed suggest that, when starting with no flow information, one event or 10 observations during high flow provide almost as much information as three months of continuously measured streamflow for constraining the calibration of a simple catchment model.

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Go to Journal of Hydrologic Engineering
Journal of Hydrologic Engineering
Volume 20Issue 1January 2015

History

Received: Oct 22, 2012
Accepted: Jun 6, 2013
Published online: Jun 8, 2013
Discussion open until: Nov 4, 2014
Published in print: Jan 1, 2015

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Dept. of Geography, Univ. of Zurich, Winterthurerstrasse 190, CH-8057 Zurich, Switzerland; Dept. of Earth Sciences, Uppsala Univ., Sweden; and Dept. of Physical Geography and Quaternary Geology, Stockholm Univ., Sweden (corresponding author). E-mail: [email protected]
J. J. McDonnell
Global Institute for Water Security, Univ. of Saskatchewan, National Hydrology Research Centre, 11 Innovation Boulevard, Saskatoon, SK, Canada S7N 3H5; and School of Geosciences, Univ. of Aberdeen, Aberdeen, UK.

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