The remarkable complexity of soil and its importance to a wide range of ecosystem services
presents major challenges to the modeling of soil processes. Although major progress in soil …

The measurement and simulation of water vapor isotopic composition has matured rapidly
over the last decade, with long‐term data sets and comprehensive modeling capabilities …

The hydrogen isotope ratio of water cryogenically extracted from plant stem samples
(δ2Hstem_CVD) is routinely used to aid isotope applications that span hydrological …

Evaporation (E) and transpiration (T) respond differently to ongoing changes in climate,
atmospheric composition, and land use. It is difficult to partition ecosystem-scale …

Renewable fresh water over continents has input from precipitation and losses to the
atmosphere through evaporation and transpiration. Global-scale estimates of transpiration …

Partitioning of evapotranspiration (ET) into evaporation from the soil (E) and transpiration
through the stomata of plants (T) is challenging but important in order to assess biomass …

Recognizing the origins and movement processes of surface water and groundwater is
crucial for understanding hydrochemical genesis, conserving water supplies, and managing …

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 …

The most important sources of atmospheric moisture at the global scale are herein identified,
both oceanic and terrestrial, and a characterization is made of how continental regions are …

Although the global partitioning of evapotranspiration (ET) into transpiration, soil
evaporation, and canopy evaporation is not well known, most current land surface schemes …