High-resolution narrowband satellite data such as Enhanced Thematic Mapper Plus (ETM+) contain important information that enables us to map land surface albedos and interrelated phenomenon in high precision. In this paper, land cover of study area is classified into three classes as to surface features so that it is less expensive to eliminate the adjacency effect and to reduce the uncertainty of angular effects caused by Lambertian surface assumption as well as spectral compensation. Then, 6S code is used to atmospheric correction of ETM+ data and to achieve spectral reflectance of different target. Next, to remedy the spectral deficiency of ETM+ data, which has only six bands could be used to calculate broadband albedo, the bandwidths not...
The broadband albedo values retrieved from satellite sensors are usually compared directly to ground...
International audienceSurface albedo can be inferred from geostationary satellite measurements as lo...
Land surface albedo is a critical variable needed in land surface modeling. The conventional method...
Surface broadband albedo is calculated from Enhanced Thematic Mapper Plus (ETM +) data using 6S (Sec...
Land surface broadband albedo is one of the most important physical parameters for climate models, b...
Land surface shortwave broadband albedo is a key parameter in general circulation models and surface...
Normalized difference vegetation index (NDVI) plays an important role in the detection of drought an...
NormaIized difference vegetation index (NDVI) plays an important role in the detection of drought an...
Surface albedo is one of the key controlling geophysical parameters in the surface energy budget stu...
Land surface albedo defines the ratio of shortwave radiation absorbed by the surface and controls th...
A method was investigated to estimate broadband surface shortwave albedo from the narrowband reflect...
[1] We describe a method to determine broadband albedo globally over land viewed by the Clouds and t...
In this paper, we propose equations for narrowband-to-broadband (NTB) albedo conversion for glacier ...
In this paper, we propose equations for narrowband-to-broadband (NTB) albedo conversion for glacier ...
The broadband albedo values retrieved from satellite sensors are usually compared directly to ground...
The broadband albedo values retrieved from satellite sensors are usually compared directly to ground...
International audienceSurface albedo can be inferred from geostationary satellite measurements as lo...
Land surface albedo is a critical variable needed in land surface modeling. The conventional method...
Surface broadband albedo is calculated from Enhanced Thematic Mapper Plus (ETM +) data using 6S (Sec...
Land surface broadband albedo is one of the most important physical parameters for climate models, b...
Land surface shortwave broadband albedo is a key parameter in general circulation models and surface...
Normalized difference vegetation index (NDVI) plays an important role in the detection of drought an...
NormaIized difference vegetation index (NDVI) plays an important role in the detection of drought an...
Surface albedo is one of the key controlling geophysical parameters in the surface energy budget stu...
Land surface albedo defines the ratio of shortwave radiation absorbed by the surface and controls th...
A method was investigated to estimate broadband surface shortwave albedo from the narrowband reflect...
[1] We describe a method to determine broadband albedo globally over land viewed by the Clouds and t...
In this paper, we propose equations for narrowband-to-broadband (NTB) albedo conversion for glacier ...
In this paper, we propose equations for narrowband-to-broadband (NTB) albedo conversion for glacier ...
The broadband albedo values retrieved from satellite sensors are usually compared directly to ground...
The broadband albedo values retrieved from satellite sensors are usually compared directly to ground...
International audienceSurface albedo can be inferred from geostationary satellite measurements as lo...
Land surface albedo is a critical variable needed in land surface modeling. The conventional method...