An Evaluation of CMIP5 GCM Simulations over the Athabasca River Basin, Canada. (28th February 2017)

• Record Type: Journal Article
• Authors: Cheng, G. H.; Huang, G. H.; Dong, C.; Zhu, J. X.; Zhou, X.; Yao, Y.
• Is Part Of: River research and applications. Volume 33:Number 5(2017)
• Page Start: 823
• Page End: 843
• Publication Date: 2017-02-28
• Subjects: CMIP5 -- Athabasca River Basin -- GCM evaluation -- Ensemble; Rivers -- Regulation -- Periodicals; Rivers -- Periodicals; 551.483
• DOI: 10.1002/rra.3136
• Languages: English
• ISSNs: 1535-1459

Abstract

Abstract: Long‐term hydrological forecasting, water resources management and other climate change impacts or adaptation analysis studies on large continental river basins, for example, the Athabasca River Basin ( ARB ) in Canada, desire a reliable climatic projection. This usually relies on general circulation models ( GCM s) in the fifth phase of the Coupled Model Intercomparison Project ( CMIP5 ). However, there is a lack of a systematic evaluation of CMIP5 GCM performances over the ARB that vary with multiple factors, for example, statistical metrics, temporal scales and spatial locations, challenging the reliability of water‐related or other studies over the ARB . For this gap to be filled, six CMIP5 GCM s, namely, IPSL‐CM5A‐LR, IPSL‐CM5A‐MR, MIROC‐ESM‐CHEM, MIROC5, GFDL‐ESM2G and GFDL‐ESM2M, and their ensemble mean are selected according to data availabilities of representative climate variables: Tmin, Tmax and Prec ( TTP ). Accuracies of the selected CMIP5 GCM s in reproducing TTP over the ARB are evaluated comprehensively. The ensemble mean cannot outperform any GCM in all cases in the ARB, although its overall accuracy seems to be higher in consideration of all cases. These accuracies vary with TTP, locations, metrics and scales. For instance, ESM2G shows the highest accuracies in reproducing monthly/seasonal variability and magnitudes of grid‐averaged TTP and inter‐annual variability of grid‐averaged annual means of Tmax ; CM5A‐LR in multi‐year‐averaged spatial variability of TTP and magnitudes of spatially distributed multi‐year‐averaged Tmax ; while the ensemble mean only in some aspects, for example, intraseasonal variability and magnitudes of TTP and inter‐annual variability and magnitudes of grid‐averaged annual means of TTP . GCM s should be systematically integrated according to accuracy variations. Multiple statistical metrics are recommended in GCM evaluations. These findings facilitate water resources systems analyses and other related studies in the ARB . Copyright © 2017 John Wiley & Sons, Ltd.