The role of evapotranspiration (ET) in the global, continental, regional, and local water
cycles is reviewed. Elevated atmospheric CO2, air temperature, vapor pressure deficit (D) …

Land cover controls the land‐atmosphere exchange of water and energy through the
partitioning of solar energy into latent and sensible heat. Observations over all land cover …

We propose a generally applicable formula for estimating evaporation rate from open water
bodies which utilizes readily available land-based meteorological data. We follow the well …

Abstract The relationship between Urban Heat Island (UHI) and energy consumption in
buildings has been widely observed and studied. The aim of this paper is to investigate the …

Abstract Study region The El Haouareb dam (Merguellil catchment) in central Tunisia, which
is typical of semi-arid environments. Study focus Most estimates of evaporation from water …

With the emergence of water supply and food security issues as a result of increasing
population and climate change pressures, the need for efficient use of available water …

Evapotranspiration is often expressed in terms of reference crop evapotranspiration (ET o),
actual evapotranspiration (ET a), or surface water evaporation (E sw), and their reliable …

In lentic water bodies, such as lakes, the water temperature near the surface typically
increases during the day, and decreases during the night as a consequence of the diurnal …

Pit lakes often form in the void that remains after open cut mining operations cease. As pit
lakes fill, hydrological and geochemical processes interact and these need to be understood …

Lake evaporation is a critical component of the hydrological cycle. Quantifying lake
evaporation in hyper-arid regions by measurement and estimation can both provide reliable …