Preprints
https://doi.org/10.5194/egusphere-2025-3062
https://doi.org/10.5194/egusphere-2025-3062
14 Jul 2025
 | 14 Jul 2025
Status: this preprint is open for discussion and under review for Hydrology and Earth System Sciences (HESS).

Revealing the Influence of Topography and Vegetation on Hydrological Processes Using a Stepwise Modelling Approach in Cold Alpine Basins of the Mongolian Plateau

Leilei Yong, Yahui Wang, Batsuren Dorjsuren, Zheng Duan, and Hongkai Gao

Abstract. Topography and vegetation are critical factors influencing catchment hydrology; however, their individual contributions are often underestimated in hydrological models. This limitation is particularly evident in cold, mountainous regions such as the Mongolian Plateau, where observational data are sparse. To address this, we employed a stepwise, top-down modelling strategy based on the FLEX framework to systematically assess the influence of topography and vegetation on hydrological processes in the Bogd Uliastai and Zavkhan Guulin river basins. Beginning with a lumped model (FLEXL), we successively integrated snow processes (FLEXL-S), topographic distribution (FLEXD), and finally, a landscape-based parameterization accounting for vegetation heterogeneity (FLEXT). Both FLEXD and FLEXT outperformed the lumped models in simulating runoff and SWE. Interestingly, FLEXT showed similar performance to FLEXD—likely due to limited vegetation heterogeneity—it offers more physically realistic parameterization by explicitly representing landscape units, suggesting its potential in more complex basins. Snowmelt contributions to streamflow were quantified as 23.5 %±1.3 % and 14.7 %±1.6 % in the Bogd Uliastai and Zavkhan Guulin river basins, respectively, with peaks in spring and a clear increase with elevation. At high elevations, delayed snowmelt resulted in sustained runoff, while lower elevations responded more rapidly to rainfall. The explicit representation of vegetation heterogeneity further improved the model’s capacity to capture landscape complexity and dominant hydrological mechanisms. This study underscores the pivotal roles of topography and vegetation in runoff generation and demonstrates the effectiveness of a stepwise modelling framework for improving hydrological understanding in cryospheric and data-scarce regions.

Competing interests: At least one of the (co-)authors is a member of the editorial board of Hydrology and Earth System Sciences.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this paper. While Copernicus Publications makes every effort to include appropriate place names, the final responsibility lies with the authors. Views expressed in the text are those of the authors and do not necessarily reflect the views of the publisher.
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Leilei Yong, Yahui Wang, Batsuren Dorjsuren, Zheng Duan, and Hongkai Gao

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Leilei Yong, Yahui Wang, Batsuren Dorjsuren, Zheng Duan, and Hongkai Gao
Leilei Yong, Yahui Wang, Batsuren Dorjsuren, Zheng Duan, and Hongkai Gao

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Short summary
Topography and vegetation critically influence hydrology but are often underrepresented in models, especially in cold, data-scarce regions like Mongolia. Using a stepwise FLEX framework, we assessed their roles in two river basins. Distributed (FLEXD) and landscape-based (FLEXT) models outperformed lumped versions. High elevations showed delayed melt sustaining flow, while low elevations responded rapidly to rain. Study confirms topography/vegetation as key hydrological controls.
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