2022
DOI: 10.5194/hess-26-3805-2022
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On the similarity of hillslope hydrologic function: a clustering approach based on groundwater changes

Abstract: Abstract. Hillslope similarity is an active topic in hydrology because of its importance in improving our understanding of hydrologic processes and enabling comparisons and paired studies. In this study, we propose a holistic bottom-up hillslope clustering based on a region's integrative hydrodynamic response quantified by the seasonal changes in groundwater levels ΔP. The main advantage of the ΔP clustering is its ability to capture recharge and discharge processes. We test the performance of the ΔP clusterin… Show more

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Cited by 2 publications
(2 citation statements)
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“…Driving force, structural elements and hydrodynamics are the three elements of hydrological similarity of watersheds, where driving force (external energy and water input) and structural elements (vegetation, topography, geology, etc.) determine the dynamics mechanism of hydrological cycle of watersheds (Maina et al, 2022; Sawicz et al, 2011). In selecting similar watersheds, we prioritized the proximity of watersheds, which, to some extent, can ensure the consistency of their driving forces (meteorological conditions) and structural elements.…”
Section: Resultsmentioning
confidence: 99%
“…Driving force, structural elements and hydrodynamics are the three elements of hydrological similarity of watersheds, where driving force (external energy and water input) and structural elements (vegetation, topography, geology, etc.) determine the dynamics mechanism of hydrological cycle of watersheds (Maina et al, 2022; Sawicz et al, 2011). In selecting similar watersheds, we prioritized the proximity of watersheds, which, to some extent, can ensure the consistency of their driving forces (meteorological conditions) and structural elements.…”
Section: Resultsmentioning
confidence: 99%
“…The TWI is an essential parameter for describing the spatial pattern of soil moisture (Li et al, 2020), which is often used to demonstrate the response of topography to hydrological processes (Maina et al, 2022; Meles et al, 2020) and the potential for possible surface runoff, calculated as follows: TWI=lnnormalAnormals/tanβ where A s is the contributing area above the analysis point and β is the cell slope.…”
Section: Methodsmentioning
confidence: 99%