Vegetation patterns governing the competitive relationship between runoff and evapotranspiration using a novel water balance model at a semi-arid watershed

Qingqing Fang; Xiaoping Xin; Tiesheng Guan; Guoqiang Wang; Shanghong Zhang; Meihong Ma

doi:10.1016/j.envres.2022.113976

Vegetation patterns governing the competitive relationship between runoff and evapotranspiration using a novel water balance model at a semi-arid watershed

Environ Res. 2022 Nov;214(Pt 4):113976. doi: 10.1016/j.envres.2022.113976. Epub 2022 Aug 20.

Authors

Qingqing Fang¹, Xiaoping Xin², Tiesheng Guan³, Guoqiang Wang⁴, Shanghong Zhang⁵, Meihong Ma⁶

Affiliations

¹ School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, 102206, China; State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing, 210029, China.
² National Hulunber Grassland Ecosystem Observation and Research Station, Institute of Agricultural, Resources and Regional Planning, Chinese Academy of Agricultural Sciences, Beijing, China.
³ State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering, Nanjing Hydraulic Research Institute, Nanjing, 210029, China; Hydrology and Water Resources Department, Nanjing Hydraulic Research Institute, Nanjing, 210029, China. Electronic address: tsguan@nhri.cn.
⁴ Hydrological Cycle and Sponge City Technology, College of Water Sciences, Beijing Normal University, Xinjiekouwai Street 19, Beijing, 100875, China.
⁵ School of Water Resources and Hydropower Engineering, North China Electric Power University, Beijing, 102206, China.
⁶ School of Geographic and Environmental Sciences, Tianjin Normal University, Tianjin, 300387, China.

PMID: 35998697
DOI: 10.1016/j.envres.2022.113976

Abstract

Vegetation patterns play an important role in precipitation partitioning into hydrological components, especially evapotranspiration and runoff. However, few studies focus on their competitive relationship and the influence of the vegetation on them. In this study, a vegetation threshold was postulated to prevent further decrease of runoff by determining a new hydrological component continuing evapotranspiration (partitioned from total and initial evapotranspiration) through a novel model coupled with the Budyko model (dimensional form) and two-stage partitioning model (nondimensional form) in the semi-arid watershed. The results showed significant correlations between model parameters ε (underlying surface index), λ (ratio of initial evapotranspiration) and vegetation coverage (M) (R² = 0.95 and 0.97, p < 0.01) b Based on the modified Budyko model and λ. The nondimensional model showed high-precise estimations of K_H (Horton index Fraction), K_B (Baseflow Fraction), K_V (evapotranspiration Fraction), K_R (runoff Fraction), and K_C (continuing evapotranspiration Fraction) (R² > 0.98, p < 0.01) as a function of a new aridity index φ. K_H, K_B, K_V, K_R, showed symmetrical patterns correlated with φ both at between-subwatershed and between-year scale based on the dimensional model and λ. However, K_C showed asymmetrical different correlation with M³ and φ (K_C/M³ ∼ φ: in between-subwatershed: R² = 0.92, p < 0.01; and between-year scale: R² = 0.74, p < 0.01). Based on the solution of continuing evapotranspiration, the vegetation threshold has been solved with M = 0.73 (+0.09/-0.02) to prevent further decreasing runoff. The framework presented can be applied in other semi-arid watersheds worldwide to better protect the sustainability of the hydro-ecosystems.

Keywords: Budyko model; Evapotranspiration; Two-stage partitioning theory; Vegetation threshold.

Publication types

Research Support, Non-U.S. Gov't

MeSH terms

Ecosystem*
Hydrology*
Water

Substances

Water