The influence of vegetation on mechanical and hydrological soil behavior represents a
significant factor to be considered in shallow landslides modelling. Among the multiple …

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 …

Forest restoration is being scaled up globally to deliver critical ecosystem services and
biodiversity benefits; however, there is a lack of rigorous comparison of cobenefit delivery …

Quantifying terrestrial evapotranspiration (ET) and soil moisture dynamics accurately is
crucial for understanding the global water cycle and surface energy balance. We present a …

This paper is a review of physically-based rainfall interception modelling. Fifteen models
were selected, representing distinct concepts of the interception process. Applications of …

A new methodology for estimating forest rainfall interception from multisatellite observations
is presented. The Climate Prediction Center morphing technique (CMORPH) precipitation …

When rain falls onto a forest a proportion is intercepted by the canopy and evaporates back
into the atmosphere, playing no further part in the terrestrial portion of the hydrologic cycle …

Depending on season, rainfall characteristics and tree species, interception amounts to 15–
50% of total precipitation in a forest under temperate climates. Many studies have …

Evaporation from wet canopies (E) can return up to half of incident rainfall back into the
atmosphere and is a major cause of the difference in water use between forests and short …

Rainfall partitioning is an important part of the ecohydrological cycle, influenced by
numerous variables. Rainfall partitioning for pine (Pinus nigra Arnold) and birch (Betula …