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Evapotranspiration partitioning at the ecosystem scale using the stable isotope method—A review
Terrestrial evapotranspiration (ET) consists of evaporation (E) from canopy-intercepted
water, evaporation from soil and open water, and transpiration (T) from plants. Determining …
water, evaporation from soil and open water, and transpiration (T) from plants. Determining …
Reviews and syntheses: Turning the challenges of partitioning ecosystem evaporation and transpiration into opportunities
Evaporation (E) and transpiration (T) respond differently to ongoing changes in climate,
atmospheric composition, and land use. It is difficult to partition ecosystem-scale …
atmospheric composition, and land use. It is difficult to partition ecosystem-scale …
[HTML][HTML] Higher soil moisture increases microclimate temperature buffering in temperate broadleaf forests
Forest canopies can buffer the understory against temperature extremes, often creating
cooler microclimates during warm summer days compared to temperatures outside the …
cooler microclimates during warm summer days compared to temperatures outside the …
[HTML][HTML] Reviews and syntheses: Gaining insights into evapotranspiration partitioning with novel isotopic monitoring methods
Y Rothfuss, M Quade, N Brüggemann, A Graf… - …, 2021 - bg.copernicus.org
Disentangling ecosystem evapotranspiration (ET) into evaporation (E) and transpiration (T)
is of high relevance for a wide range of applications, from land surface modelling to …
is of high relevance for a wide range of applications, from land surface modelling to …
Water use efficiency and its drivers in four typical agroecosystems based on flux tower measurements
Understanding the interactive responses of agroecosystem water use efficiency (WUE) to
climatic and vegetation factors is significant for revealing how ecohydrological processes …
climatic and vegetation factors is significant for revealing how ecohydrological processes …
Stable isotopes of deep soil water retain long-term evaporation loss on China's Loess Plateau
Evaporation from the land surface enriches heavy isotope ratios (2 H/1 H and 18 O/16 O) in
shallow soils, and downward water movement will carry the fractionation signal to deep …
shallow soils, and downward water movement will carry the fractionation signal to deep …
Global assessment of partitioning transpiration from evapotranspiration based on satellite solar-induced chlorophyll fluorescence data
An accurate assessment of terrestrial ecosystem transpiration (T) is important to understand
the vegetation-atmosphere feedbacks under climate change. Solar-induced chlorophyll …
the vegetation-atmosphere feedbacks under climate change. Solar-induced chlorophyll …
Effect of drip irrigation on wheat evapotranspiration, soil evaporation and transpiration in Northwest China
Drip irrigation (DI) has been widely used for corn, potato, and soybean, among other crops,
and its water-saving effect has been confirmed by numerous studies. However, how DI …
and its water-saving effect has been confirmed by numerous studies. However, how DI …
ET partitioning assessment using the TSEB model and sUAS information across california central valley vineyards
Evapotranspiration (ET) is a crucial part of commercial grapevine production in California,
and the partitioning of this quantity allows the separate assessment of soil and vine water …
and the partitioning of this quantity allows the separate assessment of soil and vine water …
Evapotranspiration partitioning for multiple ecosystems within a dryland watershed: Seasonal variations and controlling factors
Partitioning of evapotranspiration (ET) into evaporation (E) and transpiration (T) is
challenging but important to better understand the mechanisms of water loss from the …
challenging but important to better understand the mechanisms of water loss from the …