A review of global terrestrial evapotranspiration: Observation, modeling, climatology, and climatic variability
K Wang, RE Dickinson - Reviews of Geophysics, 2012 - Wiley Online Library
This review surveys the basic theories, observational methods, satellite algorithms, and land
surface models for terrestrial evapotranspiration, E (or λE, ie, latent heat flux), including a …
surface models for terrestrial evapotranspiration, E (or λE, ie, latent heat flux), including a …
Evapotranspiration estimation with small UAVs in precision agriculture
Estimating evapotranspiration (ET) has been one of the most critical research areas in
agriculture because of water scarcity, the growing population, and climate change. The …
agriculture because of water scarcity, the growing population, and climate change. The …
Calibration‐free complementary relationship estimates terrestrial evapotranspiration globally
While large‐scale terrestrial evapotranspiration (ET) information is essential for our
understanding of the Earth's water and energy cycles, substantial differences exist in current …
understanding of the Earth's water and energy cycles, substantial differences exist in current …
Complementary‐relationship‐based modeling of terrestrial evapotranspiration across China during 1982–2012: Validations and spatiotemporal analyses
N Ma, J Szilagyi, Y Zhang, W Liu - Journal of Geophysical …, 2019 - Wiley Online Library
Having recognized the limitations in spatial representativeness and/or temporal coverage of
(i) current ground ETa observations and (ii) land surface model‐and remote sensing‐based …
(i) current ground ETa observations and (ii) land surface model‐and remote sensing‐based …
Droughts in a warming climate: A global assessment of Standardized precipitation index (SPI) and Reconnaissance drought index (RDI)
Both drought and aridity indicate imbalance in water availability. While drought is a natural
temporal hazard, aridity is a constant climatic feature. This paper investigates the changes in …
temporal hazard, aridity is a constant climatic feature. This paper investigates the changes in …
Modeling reference evapotranspiration using extreme learning machine and generalized regression neural network only with temperature data
Accurate estimation of reference evapotranspiration (ET 0) is essential to agricultural water
management. The present study developed two artificial intelligence models for daily ET 0 …
management. The present study developed two artificial intelligence models for daily ET 0 …
A comprehensive evaluation of two MODIS evapotranspiration products over the conterminous United States: Using point and gridded FLUXNET and water balance …
Remote sensing datasets are increasingly being used to provide spatially explicit large
scale evapotranspiration (ET) estimates. Extensive evaluation of such large scale estimates …
scale evapotranspiration (ET) estimates. Extensive evaluation of such large scale estimates …
Separating the impacts of climate change and human activities on runoff using the Budyko-type equations with time-varying parameters
The Budyko-type equations have begun to be widely adopted to separate the contributions
of climate change and human activities to the variation of runoff over long-term periods by …
of climate change and human activities to the variation of runoff over long-term periods by …
Hybrid particle swarm optimization with extreme learning machine for daily reference evapotranspiration prediction from limited climatic data
B Zhu, Y Feng, D Gong, S Jiang, L Zhao… - Computers and Electronics …, 2020 - Elsevier
Accurate prediction of reference evapotranspiration (ET o) is pivotal to the determination of
crop water requirement and irrigation scheduling in agriculture as well as water resources …
crop water requirement and irrigation scheduling in agriculture as well as water resources …
Analysis of spatial distribution and temporal trend of reference evapotranspiration and pan evaporation in Changjiang (Yangtze River) catchment
In this study the Penman–Monteith reference evapotranspiration, pan evaporation measured
by a 20cm pan, and pan coefficient, ie, the ratio of Penman–Monteith evapotranspiration to …
by a 20cm pan, and pan coefficient, ie, the ratio of Penman–Monteith evapotranspiration to …