We analyzed the seasonal variations of energy balance components over three different surfaces: irrigated cropland (Yingke, YK), alpine meadow (A'rou, AR), and spruce forest (Guantan, GT). The energy balance components were measured using eddy covariance (EC) systems and a large aperture scintillometer (LAS) in the Heihe River Basin, China, in 2008 and 2009. We also determined the source areas of the EC and LAS measurements with a footprint model for each site and discussed the differences between the sensible heat fluxes measured with EC and LAS at AR. The results show that the main EC source areas were within a radius of 250 m at all of the sites. The main source area for the LAS (with a path length of 2390 m) stretched along a path line ...
In much of the western US, mountain regions store water in the snowpack, and contain ecosystems that...
Quantitative knowledge of the surface energy balance is essential for the prediction of weather and ...
The eddy covariance and energy balance method was employed to determine evapotranspiration (LE) over...
Network of eddy covariance observation is measuring long-term carbon and water fluxes in contrasting...
The sensible heat is an important component in surface energy partitioning over the land surface. Th...
The surface energy budget at the earth surface describes the partitioning of energy into storage (S)...
AbstractThe use of energy fluxes data to validate land surface models requires that energy balance c...
Scintillometry is an established technique for determining large areal average sensible heat fluxes....
The accuracy of the components of the surface energy balance were analysed, in an attempt to determ...
The use of energy fluxes data to validate land surface models requires that energy balance closure c...
The Eddy Covariance (EC) technique is used worldwide to monitor gas and energy exchanges at the inte...
The eddy covariance (EC) technique is generally regarded as a standard method for crop evapotranspir...
The energy observed in the surface layer, when using eddy-covariance techniques to measure turbulent...
The unresolved energy-unclosed problem in micrometeorology refers to the fact that the sum of turbul...
The apparent lack of surface energy balance closure is one of the most crucial challenges in the mea...
In much of the western US, mountain regions store water in the snowpack, and contain ecosystems that...
Quantitative knowledge of the surface energy balance is essential for the prediction of weather and ...
The eddy covariance and energy balance method was employed to determine evapotranspiration (LE) over...
Network of eddy covariance observation is measuring long-term carbon and water fluxes in contrasting...
The sensible heat is an important component in surface energy partitioning over the land surface. Th...
The surface energy budget at the earth surface describes the partitioning of energy into storage (S)...
AbstractThe use of energy fluxes data to validate land surface models requires that energy balance c...
Scintillometry is an established technique for determining large areal average sensible heat fluxes....
The accuracy of the components of the surface energy balance were analysed, in an attempt to determ...
The use of energy fluxes data to validate land surface models requires that energy balance closure c...
The Eddy Covariance (EC) technique is used worldwide to monitor gas and energy exchanges at the inte...
The eddy covariance (EC) technique is generally regarded as a standard method for crop evapotranspir...
The energy observed in the surface layer, when using eddy-covariance techniques to measure turbulent...
The unresolved energy-unclosed problem in micrometeorology refers to the fact that the sum of turbul...
The apparent lack of surface energy balance closure is one of the most crucial challenges in the mea...
In much of the western US, mountain regions store water in the snowpack, and contain ecosystems that...
Quantitative knowledge of the surface energy balance is essential for the prediction of weather and ...
The eddy covariance and energy balance method was employed to determine evapotranspiration (LE) over...