Soil moisture (SM) is an essential parameter for understanding the interactions and
feedbacks between the atmosphere and the Earth's surface through energy and water …

Evapotranspiration is a major component of the global water cycle and provides a critical
nexus between terrestrial water, carbon and surface energy exchanges. Evapotranspiration …

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 …

This paper reviews methods for estimating evaporation from landscapes, regions and larger
geographic extents, with remotely sensed surface temperatures, and highlights uncertainties …

An overview of the commonly applied evapotranspiration (ET) models using remotely
sensed data is given to provide insight into the estimation of ET on a regional scale from …

Accurate estimation of spatially distributed air temperature (Ta) is useful for a wide range of
disciplines such as hydrology, meteorology and ecology. Moderate Resolution Imaging …

Multispectral imagery has been used as the data source for water and land observational
remote sensing from airborne and satellite systems since the early 1960s. Over the past two …

Three process based models are used to estimate terrestrial heat fluxes and
evapotranspiration (ET) at the global scale: a single source energy budget model, a Penman …

Soil moisture availability affects rainfed crop yield. Therefore, the development of methods
for pre-harvest yield prediction is essential for the food security. A study was carried out to …

The commonly applied surface temperature–vegetation index (Ts–VI) triangle method is
used to estimate regional evapotranspiration (ET) in arid and semi-arid regions. A practical …