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Worldwide evaluation of mean and extreme runoff from six global-scale hydrological models that account for human impacts

Zaherpour, Jamal; Gosling, Simon N.; Mount, Nick J.; Müller Schmied, Hannes; Veldkamp, Ted; Dankers, Rutger; Eisner, Stephanie; Gerten, Dieter; Gudmundsson, Lukas; Haddeland, I.; Hanasaki, Naota; Kim, Hyungjun; Leng, Guoyong; Liu, Junguo; Masaki, Yoshimitsu; Oki, Taikan; Pokhrel, Yadu; Satoh, Yusuke; Schewe, Jacob; Wada, Yoshihide

Authors

Jamal Zaherpour lgxjz1@nottingham.ac.uk

Simon N. Gosling

Nick J. Mount nick.mount@nottingham.ac.uk

Hannes Müller Schmied

Ted Veldkamp

Rutger Dankers

Stephanie Eisner

Dieter Gerten

Lukas Gudmundsson

I. Haddeland

Naota Hanasaki

Hyungjun Kim

Guoyong Leng

Junguo Liu

Yoshimitsu Masaki

Taikan Oki

Yadu Pokhrel

Yusuke Satoh

Jacob Schewe

Yoshihide Wada



Abstract

Global-scale hydrological models are routinely used to assess water scarcity, flood hazards and droughts worldwide. Recent efforts to incorporate anthropogenic activities in these models have enabled more realistic comparisons with observations. Here we evaluate simulations from an ensemble of six models participating in the second phase of the Inter-Sectoral Impact Model Inter-comparison Project (ISIMIP2a). We simulate observed monthly runoff in 40 catchments, spatially distributed across 8 global hydrobelts. The performance of each model and the ensemble mean is examined with respect to their ability to replicate observed mean and extreme runoff under human-influenced conditions. Application of
a novel integrated evaluation metric to quantify the models’ ability to simulate timeseries of monthly runoff suggests that the models generally perform better in the wetter equatorial and northern hydrobelts than in drier southern hydrobelts. When model outputs are temporally aggregated to assess mean annual and extreme runoff, the models perform better. Nevertheless, we find a general trend in the majority of models towards the overestimation of mean annual runoff and all
indicators of upper and lower extreme runoff. There are particular challenges associated with reproducing both the timing and magnitude of seasonal cycles; the models struggle to capture the timing of the seasonal cycle, particularly in northern hydrobelts, while in southern hydrobelts the models struggle to reproduce the magnitude of the seasonal cycle. It is noteworthy that over all hydrological indicators, the ensemble mean fails to perform better than any individual model – a
finding that challenges the commonly held perception that model ensemble estimates deliver superior performance over individual models. The study highlights the need for continued model development and improvement. It also suggests that caution should be taken when summarising the simulations from a model ensemble based upon its mean output.

Journal Article Type Article
Publication Date Jun 12, 2018
Journal Environmental Research Letters
Electronic ISSN 1748-9326
Publisher IOP Publishing
Peer Reviewed Peer Reviewed
Volume 13
Issue 6
APA6 Citation Zaherpour, J., Gosling, S. N., Mount, N. J., Müller Schmied, H., Veldkamp, T., Dankers, R., …Wada, Y. (2018). Worldwide evaluation of mean and extreme runoff from six global-scale hydrological models that account for human impacts. Environmental Research Letters, 13(6), https://doi.org/10.1088/1748-9326/aac547
DOI https://doi.org/10.1088/1748-9326/aac547
Keywords global hydrological models, land surface models, human impacts, extreme events, model evaluation, model validation
Publisher URL http://iopscience.iop.org/article/10.1088/1748-9326/aac547
Copyright Statement Copyright information regarding this work can be found at the following address: http://creativecommons.org/licenses/by/4.0

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Copyright Statement
Copyright information regarding this work can be found at the following address: http://creativecommons.org/licenses/by/4.0


Zaherpour_2018_Environ._Res._Lett._13_065015.pdf (4.3 Mb)
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