Abstract: This study highlights the possibilities and constraints of determining instantaneous spatial surface radiation and land heat fluxes from satellite images in a heterogeneous urban area and its agricultural and natural surroundings. Net radiation was determined using ASTER satellite data and MODTRAN radiative transfer calculations. The soil heat flux was estimated with two empirical methods using radiative terms and vegetation indices. The turbulent heat fluxes finally were determined with the LUMPS (Local-Scale Urban Meteorological Parameterization Scheme) and the ARM (Aerodynamic Resistance Method) method. Results were compared to in situ measured ground data. The performance of the atmospheric correction was found to be crucial f...
The impacts of climate change and also the modification of the urban climate of the cities itself ca...
This paper describes a modified version of the Surface Energy Balance System (SEBS) as regards the u...
Land cover has a strong effect on the evapotranspiration (ET) and the hydrologic cycle. Urbanization...
This study highlights the possibilities and constraints of determining instantaneous spatial surface...
Accurate estimation of surface energy fluxes from space at high spatial resolution has the potential...
Land surface heat fluxes are essential measures of the strengths of land-atmosphere interactions inv...
Using ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) infrared remote sensing...
The urban heat island phenomenon occurs as a mixed result of anthropogenic heat discharge, decreased...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Current urban/rural surface energy balance simulations using boundary layer climate models have been...
Copyright © 2014 ISSR Journals. This is an open access article distributed under the Creative Common...
Reliably estimating the turbulent fluxes of latent and sensible heat at the Earth’s surface by remot...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Urban areas have discrete differences in their land surface temperatures (LST) compared to rural are...
The impacts of climate change and also the modification of the urban climate of the cities itself ca...
This paper describes a modified version of the Surface Energy Balance System (SEBS) as regards the u...
Land cover has a strong effect on the evapotranspiration (ET) and the hydrologic cycle. Urbanization...
This study highlights the possibilities and constraints of determining instantaneous spatial surface...
Accurate estimation of surface energy fluxes from space at high spatial resolution has the potential...
Land surface heat fluxes are essential measures of the strengths of land-atmosphere interactions inv...
Using ASTER (Advanced Spaceborne Thermal Emission and Reflection Radiometer) infrared remote sensing...
The urban heat island phenomenon occurs as a mixed result of anthropogenic heat discharge, decreased...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Current urban/rural surface energy balance simulations using boundary layer climate models have been...
Copyright © 2014 ISSR Journals. This is an open access article distributed under the Creative Common...
Reliably estimating the turbulent fluxes of latent and sensible heat at the Earth’s surface by remot...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Accurate quantification of the amount and spatial variation of evapotranspiration is important in a ...
Urban areas have discrete differences in their land surface temperatures (LST) compared to rural are...
The impacts of climate change and also the modification of the urban climate of the cities itself ca...
This paper describes a modified version of the Surface Energy Balance System (SEBS) as regards the u...
Land cover has a strong effect on the evapotranspiration (ET) and the hydrologic cycle. Urbanization...