Preprints
https://doi.org/10.5194/hess-2024-89
https://doi.org/10.5194/hess-2024-89
12 Jul 2024
 | 12 Jul 2024
Status: this preprint is currently under review for the journal HESS.

Merits and Limits of SWAT-GL: Application in Contrasting Glaciated Catchments

Timo Schaffhauser, Florentin Hofmeister, Gabriele Chiogna, Fabian Merk, Ye Tuo, Julian Machnitzke, Lucas Alcamo, Jingshui Huang, and Markus Disse

Abstract. The recently released SWAT-GL aims to overcome multiple limitations of the traditional hydrological model SWAT (Soil Water Assessment Tool) in glaciated mountainous catchments. SWAT-GL intends to increase the applicability of SWAT in these catchments and to reduce misapplication when glaciers have a significant role in the catchment hydrology. It thereby relies on a mass balance module, based on a degree-day approach similar to SWAT’s snow melt module, extended by a glacier evolution component which is based on the delta-h (Δh) parameterization. The latter one is a mass conserving approach which enables the spatial distribution of ice thickness changes and thus dynamic glacier retreat. However, the extended SWAT version was not yet comprehensively assessed. Hence, our paper aims to evaluate SWAT-GL using four different benchmark glaciers which are part of the USGS (United States Geological Survey) Benchmark Glacier Project. The study considers a comprehensive evaluation procedure, where the routine is optimized on glacier mass balance and hypsometry as well as snow cover. Snow cover is included to consider snow-glacier feedbacks appropriately. Besides, a sensitivity analysis using Elementary Effects (or Method of Morris) is performed to give a detailed picture on the importance of the introduced glacier processes, as well as the relevance of the interactions with the already-existing snow routine. We intentionally did not include discharge in the optimization procedure to fully demonstrate the capabilities of SWAT-GL in terms of glacier and snow processes. Results demonstrate that SWAT-GL is able to perform reasonably well in contrasting glaciated catchments, which underlines SWAT-GL’s applicability and transferability. We could further show its strong (non-linear) interactions with the existing snow routine suggesting a simultaneous calibration of the snow components. While snow and glacier processes were adequately represented in the catchments, discharge was not necessarily represented sufficiently when excluded in the optimization procedure. However, SWAT-GL has been shown to be easily capable of reproducing discharge when used in a stand-alone optimization, although this may come at the expense of model consistency.

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Timo Schaffhauser, Florentin Hofmeister, Gabriele Chiogna, Fabian Merk, Ye Tuo, Julian Machnitzke, Lucas Alcamo, Jingshui Huang, and Markus Disse

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on hess-2024-89', Cyril Thébault, 09 Aug 2024
  • RC2: 'Comment on hess-2024-89', Anonymous Referee #2, 20 Sep 2024
  • RC3: 'Comment on hess-2024-89', Dipti Tiwari, 17 Oct 2024
Timo Schaffhauser, Florentin Hofmeister, Gabriele Chiogna, Fabian Merk, Ye Tuo, Julian Machnitzke, Lucas Alcamo, Jingshui Huang, and Markus Disse
Timo Schaffhauser, Florentin Hofmeister, Gabriele Chiogna, Fabian Merk, Ye Tuo, Julian Machnitzke, Lucas Alcamo, Jingshui Huang, and Markus Disse

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Short summary
The glacier-expanded SWAT version, SWAT-GL, was tested in four different catchments. The assessment highlighted the capabilities of the glacier routine. It was evaluated based on the representation of glacier mass balance, snow cover and glacier hypsometry. It was shown that glacier changes over a long time scale could be adequately represented, leading to promising potential future applications in glaciated and high mountain environments.