The changes in Amazonian landscape are determinants and able to result in significant implications in physical processes, biota and regional climate, therefore, evaluate the aspects concerning the flows on the surface in different regions of this biome is essential to understanding the possible effects of changes in land use. However, due to its vast extent, measures of surface at various points of the Amazon are hampered, requiring a tool more viable and less costly. Thus, aiming to validate a methodology for determination of microclimatic parameters and support future applications in studies of impacts of land use change in the Amazon region, this study estimated the radiation balance in a forest area located in Southwest Amazonia, throug...
This is the final version of the article. Available from the publisher via the DOI in this record.In...
Atmospheric long wave radiation (Lin) is the most difficult component of the radiation budget to be ...
Spatial variability of surface energy and water fluxes at local scales is strongly controlled by soi...
Changes in land use have motivated research on the dynamics of radiative and energy exchange in the ...
O principal objetivo deste estudo foi analisar de forma comparativa a estimativa do saldo de radiaç...
The surface radiation balance is the balance between radiation that incoming and the radiation radia...
In the Amazon region, the estimation of radiation fluxes through remote sensing techniques is hinder...
Deforestation in the Amazon region will initially impact the energy balance at the land surface thro...
Micrometerological observations have been used to study the radiation balance over recultivation are...
The southwest area of the Brazilian Amazon is composed of a landscape mosaic with transition grassla...
Este estudo tem como objetivo estimar os componentes do balanço de radiação em duas regiões do estad...
O albedo é definido como a razão entre a radiação solar refletida e a radiação solar incidente em um...
Land use and land cover is essential in regulating the water cycle and influences the evapotranspira...
O presente trabalho teve por objetivos estimar os componentes do balanço de energia à superfície e ...
The evapotranspiration (ET) was spatialized using SEBAL algorithm for a region of primary forest in ...
This is the final version of the article. Available from the publisher via the DOI in this record.In...
Atmospheric long wave radiation (Lin) is the most difficult component of the radiation budget to be ...
Spatial variability of surface energy and water fluxes at local scales is strongly controlled by soi...
Changes in land use have motivated research on the dynamics of radiative and energy exchange in the ...
O principal objetivo deste estudo foi analisar de forma comparativa a estimativa do saldo de radiaç...
The surface radiation balance is the balance between radiation that incoming and the radiation radia...
In the Amazon region, the estimation of radiation fluxes through remote sensing techniques is hinder...
Deforestation in the Amazon region will initially impact the energy balance at the land surface thro...
Micrometerological observations have been used to study the radiation balance over recultivation are...
The southwest area of the Brazilian Amazon is composed of a landscape mosaic with transition grassla...
Este estudo tem como objetivo estimar os componentes do balanço de radiação em duas regiões do estad...
O albedo é definido como a razão entre a radiação solar refletida e a radiação solar incidente em um...
Land use and land cover is essential in regulating the water cycle and influences the evapotranspira...
O presente trabalho teve por objetivos estimar os componentes do balanço de energia à superfície e ...
The evapotranspiration (ET) was spatialized using SEBAL algorithm for a region of primary forest in ...
This is the final version of the article. Available from the publisher via the DOI in this record.In...
Atmospheric long wave radiation (Lin) is the most difficult component of the radiation budget to be ...
Spatial variability of surface energy and water fluxes at local scales is strongly controlled by soi...