Mapping in situ eddy covariance measurements of terrestrial land–atmosphere fluxes to the
globe is a key method for diagnosing the Earth system from a data-driven perspective. We …

Hostile climatic conditions, including high water deficit in the soil-atmosphere system
characterize regions with arid and semi-arid climates. Local landscapes with climates of low …

The FLUXNET network with numerous eddy covariance stations distributed worldwide is an
important backbone for the study of ecosystem-atmosphere interactions. In order to provide …

Latent and sensible heat flux observations are essential for understanding land–atmosphere
interactions. Measurements from the eddy covariance technique are widely used but suffer …

Evaporative loss of interception (E i) is the first process occurring during rainfall, yet its role
in large-scale surface water balance has been largely underexplored. Here we show that E i …

A good understanding of land-atmosphere exchange processes is essential for developing
sustainable land management practices in Africa, in order to enhance food security and …

The variability and drivers of carbon and water fluxes and their relationship to ecosystem
water use efficiency (WUE) in natural ecosystems of southern South America are still poorly …

Evapotranspiration (ET) plays a critical role in water and energy budgets at regional to
global scales. ET is composed of direct evaporation (E) and plant transpiration (T) where the …

Actual evapotranspiration (ET a) is an essential variable in linking energy cycles, carbon,
and water, yet challenging to measure. Inputs uncertainty and deficiencies in the key …

Partitioning of evapotranspiration (ET) in urban forest lands plays a vital role in mitigating
ambient temperature and evaluating the effects of urbanization on the urban hydrological …