Diagnosing Hydrological Process Controls in Streamflow Generation and Variability in a 1 Glacierized Alpine Headwater Basin

This is the peer reviewed version of the following article: Aubry-Wake, C., Pradhananga, D., Pomeroy, J. W. (2022). Diagnosing Hydrological Process Controls in Streamflow Generation and Variability in a 1 Glacierized Alpine Headwater Basin. Hydrological Processess, Volume36, Issue10. https://doi.org...

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Bibliographic Details
Published in:Hydrological Processes
Main Authors: Aubry-Wake, Caroline, Pradhananga, Dhiraj, Pomeroy, John
Format: Article in Journal/Newspaper
Language:English
Published: Wiley Online Library 2022
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Online Access:https://hdl.handle.net/10388/14923
https://doi.org/10.1002/hyp.14731
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Summary:This is the peer reviewed version of the following article: Aubry-Wake, C., Pradhananga, D., Pomeroy, J. W. (2022). Diagnosing Hydrological Process Controls in Streamflow Generation and Variability in a 1 Glacierized Alpine Headwater Basin. Hydrological Processess, Volume36, Issue10. https://doi.org/10.1002/hyp.14731, which has been published in final form at https://doi.org/10.1002/hyp.14731. This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions. This article may not be enhanced, enriched or otherwise transformed into a derivative work, without express permission from Wiley or by statutory rights under applicable legislation. Copyright notices must not be removed, obscured or modified. The article must be linked to Wiley’s version of record on Wiley Online Library and any embedding, framing or otherwise making available the article or pages thereof by third parties from platforms, services and websites other than Wiley Online Library must be prohibited. Natural Sciences Engineering and Research Council of Canada, Vanier and Michael Smith Scholarships, Canada Foundation for Innovation, Canada Research Chairs, Canada First Research Excellence Fund, Global Water Futures Peer Reviewed Mountain glacierized headwaters are currently witnessing a transient shift in their hydrological and glaciological systems in response to rapid climate change. To characterize these changes, a robust understanding of the hydrological processes operating in the basin and their interactions is needed. Such an investigation was undertaken in the Peyto Glacier Research Basin, Canadian Rockies over 32 years (1988–2020). A distributed, physically based, uncalibrated glacier hydrology model was developed using the modular, object-oriented Cold Region Hydrological Modelling Platform to simulate both on and off-glacier high mountain processes and streamflow generation. The hydrological processes that generate streamflow from this alpine basin are characterized ...