This work studied the behavior and seasonality of evapotranspiration influenced by biotic and abiotic factors through analysis of diurnal variation of aerodynamic resistance (ra), stomatal resistance (rs) and decoupling factor (Ω). This index was proposed by Jarvis and McNaughton (1986) as an indicative of the control of these resistances on the evapotranspiration of vegetation. Selection of representative data from wet and dry seasons from a primary forest in Central Amazonia and a primary forest and a pasture sites in Southwestern Amazonia had shown that: (i) ra is about 20 s.m-1 in both forests in both seasons, and ranges from 70 to 100 s.m-1 in the pasture site; (ii) rs varies both throughout the day and seasonally, with medians increas...
A micrometeorological experiment was conducted over grasslands in a semi-arid region ...
Knowledge on evapotranspiration is essential in quantifying water use depletion and to allocate scar...
Comparative measurements of radiation flux components and turbulent fluxes of energy and CO2 are mad...
This work studied the behavior and seasonality of evapotranspiration influenced by biotic and abioti...
This work studied the behavior and seasonality of evapotranspiration influenced by biotic and abioti...
This study analyzes evapotranspiration data for three wet and two seasonally dry rain forest sites i...
This article discusses seasonal and interannual variations of the evapotranspiration (ET) rates in B...
In the present work we study the seasonal variation of the transpiration of a tropical forest, and i...
We used the eddy covariance technique from July 2000 to July 2001 to measure the fluxes of sensible ...
Canopy and aerodynamic conductances (g(C) and g(A)) are two of the key land surface biophysical vari...
Considering the high rates of evapotranspiration of Amazonian forests, understanding the impacts of ...
The extent to which soil water storage can support an average dry season evapotranspiration (ET) is ...
We investigated the seasonal patterns of water vapor and sensible heat flux along a tropical biome g...
We investigated the seasonal patterns of water vapor and sensible heat flux along a tropical biome g...
A micrometeorological experiment was conducted over grasslands in a semi-arid region of north-easter...
A micrometeorological experiment was conducted over grasslands in a semi-arid region ...
Knowledge on evapotranspiration is essential in quantifying water use depletion and to allocate scar...
Comparative measurements of radiation flux components and turbulent fluxes of energy and CO2 are mad...
This work studied the behavior and seasonality of evapotranspiration influenced by biotic and abioti...
This work studied the behavior and seasonality of evapotranspiration influenced by biotic and abioti...
This study analyzes evapotranspiration data for three wet and two seasonally dry rain forest sites i...
This article discusses seasonal and interannual variations of the evapotranspiration (ET) rates in B...
In the present work we study the seasonal variation of the transpiration of a tropical forest, and i...
We used the eddy covariance technique from July 2000 to July 2001 to measure the fluxes of sensible ...
Canopy and aerodynamic conductances (g(C) and g(A)) are two of the key land surface biophysical vari...
Considering the high rates of evapotranspiration of Amazonian forests, understanding the impacts of ...
The extent to which soil water storage can support an average dry season evapotranspiration (ET) is ...
We investigated the seasonal patterns of water vapor and sensible heat flux along a tropical biome g...
We investigated the seasonal patterns of water vapor and sensible heat flux along a tropical biome g...
A micrometeorological experiment was conducted over grasslands in a semi-arid region of north-easter...
A micrometeorological experiment was conducted over grasslands in a semi-arid region ...
Knowledge on evapotranspiration is essential in quantifying water use depletion and to allocate scar...
Comparative measurements of radiation flux components and turbulent fluxes of energy and CO2 are mad...