Preprints
https://doi.org/10.5194/hess-2024-136
https://doi.org/10.5194/hess-2024-136
17 Jun 2024
 | 17 Jun 2024
Status: this preprint is currently under review for the journal HESS.

Evaluating the effects of topography and land use change on hydrological signatures: a comparative study of two adjacent watersheds

Haifan Liu, Haochen Yan, and Mingfu Guan

Abstract. Watershed hydrological processes are significantly influenced by land use/land cover change (LULCC) and watershed characteristics such as topography. This study comparatively investigates the impacts of terrain slope and urbanization-driven LULCC on hydrological processes in two adjacent subtropical watersheds but with distinct terrain and land-cover conditions within the Greater Bay Area (GBA) of China. We developed an Integrated Surface-Subsurface Hydrological Model (ISSHM) using the Simulator for Hydrologic Unstructured Domains (SHUD), which was calibrated using data from river and groundwater flow monitoring stations in the watersheds. The calibrated model facilitated simulations to assess how terrain slope and LULCC affect surface runoff, subsurface flow, evapotranspiration (ET), and infiltration. Our results indicate that slope impacts hydrological processes differently in watersheds with varying characteristics. In mountainous areas, there are consistent high correlations between slope and annual surface runoff, infiltration, and subsurface flow across all watersheds. However, at lower elevations, the hydrological responses of steeper watersheds correlate weakly with local slope. Furthermore, urbanization (increase in impervious areas) has led to significant increases in annual surface runoff and significant decreases in annual infiltration and ET across all watersheds, especially in those with steeper slopes. On the other hand, in watersheds with gentler slopes, the annual increase in surface runoff is less than the percentage increase in impervious area, suggesting a buffering capacity of these flatter watersheds against urbanization. However, this buffering capacity is diminishing with increasing annual rainfall intensity.

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Haifan Liu, Haochen Yan, and Mingfu Guan

Status: open (until 19 Aug 2024)

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Haifan Liu, Haochen Yan, and Mingfu Guan
Haifan Liu, Haochen Yan, and Mingfu Guan

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Short summary
In mountainous areas, the relationship between slope and annual hydrological processes is pronounced. However, at lower elevations, this relationship is weak in steeper watersheds. In addition, urbanization leads to an increase in annual surface runoff in all watersheds, especially in steep-slope watersheds. Flatter watersheds exhibit a buffering capacity against urbanization. However, this buffering capacity is diminishing as annual rainfall intensity increases.