1. Distribution of evapotranspiration components along vertical layers and their controls in dry days of larch plantation in the Liupan Mountains of northwest China.
- Author
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Yu, Songping, Liu, Zebin, Guo, Jianbin, Wang, Yanhui, Yu, Pengtao, Xu, Lihong, Wang, Yubing, and Chao, Yang
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LEAF area index , *FOREST management , *SOIL moisture , *WATER management , *EVAPOTRANSPIRATION - Abstract
• Quantification of vertical distribution of evapotranspiration (ET f) components along forest layers. • A systematic evapotranspiration model reflecting the impacts of forest layer structure. • Higher accuracy and local applicability of new evapotranspiration model compared to conventional model. Precise quantification of forest evapotranspiration (ET f) including transpiration from tree (T t), shrub (T s), and herb (T h) layers, as well as evaporation from litter (E l) and soil (E s) layers, and elucidating their responses to environmental conditions and stand structures are crucial for forest water management in water-limited forests. In this study, we observed the T t , T s , T h , E l , and E s , reference evapotranspiration (ET o), soil volumetric water content (SWC), litter water content (LWC), leaf area index (LAI) in tree, shrub, and herb layers, and canopy shade (K sc) from tree layer of the Larix principis-rupprechtii plantation during the dry days from May to October of 2021 and 2022 to elucidate the distribution of evapotranspiration along vertical layers and their environmental and structural determinants. The results indicated that the contributions of T t , T s , T h , E l , and E s to ET f during the dry days in 2021 (2022) were 42.1 % (44.7 %), 9.2 % (8.1 %), 8.2 % (8.6 %), 15.0 % (13.1 %), and 25.5 % (25.5 %), respectively. Although T t and T s demonstrated quadratic relationships with ET o , T h , E l , and E s exhibited linear relationships. All ET c s demonstrated a saturated exponential relationship with either SWC or LWC. Furthermore, T t , T s , and T h showed a saturated exponential relationship with their respective LAI, whereas E l and E s exhibited a cubic relationship with LAI in tree layers. All understory ET c s (T s , T h , E l , and E s) decreased exponentially with the K sc. The multi-factor models of evapotranspiration component (ET c) from different vertical layers, which coupled the impacts of environmental conditions and vertical structure, were developed, and provided superior accuracy (R2 = 0.78–0.88, NSE = 0.78–0.86, RSME = 0.03–0.16). Such insights deepened the understanding of vertical structural distribution and multi-factor responses of ET c s in forest ecosystems and hold the potential to inform and optimise forest water management strategies. [Display omitted] [ABSTRACT FROM AUTHOR]
- Published
- 2024
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