Articles | Volume 19, issue 10
Hydrol. Earth Syst. Sci., 19, 4127–4147, 2015
https://doi.org/10.5194/hess-19-4127-2015
Hydrol. Earth Syst. Sci., 19, 4127–4147, 2015
https://doi.org/10.5194/hess-19-4127-2015

Research article 13 Oct 2015

Research article | 13 Oct 2015

Effects of hydrologic conditions on SWAT model performance and parameter sensitivity for a small, mixed land use catchment in New Zealand

W. Me et al.

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Cited articles

Abbaspour, K. C.: SWAT-CUP: SWAT Calibration and Uncertainty Programs – A User Manual, Open File Rep., Eawag, Swiss Federal Institute of Aquatic Science and Technology, Dübendorf, Switzerland, 100 pp., 2015.
Abbaspour, K. C., Johnson, C. A., and van Genuchten, M. Th.: Estimating uncertain flow and transport parameters using a sequential uncertainty fitting procedure, Vadose Zone J., 3, 1340–1352, https://doi.org/10.2136/vzj2004.1340, 2004.
Abbaspour, K. C., Yang, J., Maximov, I., Siber, R., Bogner, K., Mieleitner, J., Zobrist, J., and Srinivasan, R.: Modelling hydrology and water quality in the pre-alpine/alpine Thur watershed using SWAT, J. Hydrol., 333, 413–430, https://doi.org/10.1016/j.jhydrol.2006.09.014, 2007.
Abell, J. M. and Hamilton, D. P.: Bioavailability of phosphorus transported during storm flow to a eutrophic, polymictic lake, New Zeal. J. Mar. Fresh., 47, 481–489, https://doi.org/10.1080/00288330.2013.792851, 2013.
Abell, J. M., Hamilton, D. P., and Rutherford, J. C.: Quantifying temporal and spatial variations in sediment, nitrogen and phosphorus transport in stream inflows to a large eutrophic lake, Environ. Sci.: Processes Impacts, 15, 1137–1152, https://doi.org/10.1039/c3em00083d, 2013.
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Short summary
This study examined the applicability of the SWAT model to a moderately steep, temperate, small–sized catchment in Rotorua, New Zealand. It highlighted the importance of using high–frequency, event–based monitoring data for model calibration to alleviate the potential of underestimation of storm–driven fluxes. Parameter sensitivity was quantified for discharge, sediment and nutrient fluxes dependent on the relative dominance of base flow and quick flow.