Evapotranspiration partitioning, stomatal conductance, and components of the water balance: A special case of a desert ecosystem in China

Publication Type:
Journal Article
Journal of Hydrology, 2016, 538 pp. 374 - 386
Issue Date:
Full metadata record
Files in This Item:
Filename Description Size
Partitioning ET in a chinese desert J Hydrol May 2016.pdfPublished Version2.15 MB
Adobe PDF
© 2016 Elsevier B.V. Partitioning evapotranspiration (ET) into its components reveals details of the processes that underlie ecosystem hydrologic budgets and their feedback to the water cycle. We measured rates of actual evapotranspiration (ETa), canopy transpiration (Tc), soil evaporation (Eg), canopy-intercepted precipitation (EI), and patterns of stomatal conductance of the desert shrub Calligonum mongolicum in northern China to determine the water balance of this ecosystem. The ETawas 251 ± 8 mm during the growing period, while EI, Tc, and Egaccounted for 3.2%, 63.9%, and 31.3%, respectively, of total water use (256 ± 4 mm) during the growing period. In this unique ecosystem, groundwater was the main water source for plant transpiration and soil evaporation, Tcand exceeded 60% of the total annual water used by desert plants. ET was not sensitive to air temperature in this unique desert ecosystem. Partitioning ET into its components improves our understanding of the mechanisms that underlie adaptation of desert shrubs, especially the role of stomatal regulation of Tcas a determinant of ecosystem water balance.
Please use this identifier to cite or link to this item: