img

Wechat

Adv search

Journal of Desert Research ›› 2025, Vol. 45 ›› Issue (6): 289-299.DOI: 10.7522/j.issn.1000-694X.2025.00057

Previous Articles    

Evaporative fractions and soil moisture thresholds in typical vegetation types of arid and semi-arid regions

Haixian Wang1,2(), Yongyong Zhang1,2(), Wenrong Kang1,2, Jianhua Xiao1,2, Shumin Wang1,2, Shue Wei1,2, Shaoxiong Wu3   

  1. 1.Linze Inland River Basin Research Station,Chinese Ecosystem Research Network / State Key Laboratory of Ecological Safety and Sustainable Development in Arid Lands,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    2.University of Chinese Academy of Sciences,Beijing 100049,China
    3.Jingdezhen Meteorological Bureau,Jingdezhen 333000,Jiangxi,China
  • Received:2025-01-20 Revised:2025-03-13 Online:2025-11-20 Published:2025-11-26
  • Contact: Yongyong Zhang

Abstract:

To investigate the seasonal dynamics of evapotranspiration fraction (EF) in typical vegetation types and its response mechanisms to soil moisture and meteorological factors in arid and semi-arid regions, this study utilized long-term observational data from 24 FLUXNET sites representing four vegetation types (woody savanna, savanna, open shrubland, and grassland). Classical statistical methods were employed to quantify EF characteristics and its influencing factors, while threshold regression models combined with the Akaike Information Criterion (AIC) were applied to identify soil moisture thresholds and optimal fitting models. The results demonstrated that the monthly mean EF in arid and semi-arid regions was 0.31, with the highest value observed in woody savanna (0.36) and the lowest in open shrubland (0.21), indicating energy partitioning dominated by sensible heat flux. EF exhibited pronounced seasonal variability, with open shrubland showing the strongest fluctuations (Cv = 0.37). Soil moisture emerged as the key regulatory factor for EFr = 0.66, P < 0.05), with nonlinear threshold effects: the response patterns of EF to soil moisture diverged significantly before and after critical thresholds (4.73%-15.98%), and the "stepwise segmented" model was consistently identified as the optimal fitting model.

Key words: arid and semi-arid regions, evaporative fraction, soil moisture, soil moisture threshold

CLC Number: