The aerodynamic roughness length Z0, the zero-plane displacement d, the momentum drag coefficient CD, water and heat drag coefficient CH calculated by using turbulence data and wind, temperature profile data observed in Changbai Mountain forest. The causes of the error in the method of calculating d and Z0 are also discussed. The method based on the mass conservation principle is a practical one to calculate the aerodynamic roughness length and zero-plane displacement over tall vegetations. In Changbai Mountain forest, the roughness length Z0 is about 1.6&plusmn0.25 m and the zero-plane displacement d is about 19.5&plusmn1.38 m. Drag coefficients CD and CH have a good relation with stability under unstable condition, and the average...
Aerodynamic roughness height (Zom) is a key parameter required in several land surface hydrological ...
The displacement height d and roughness length z0 are parameters of the logarithmic wind profile and...
<p>The parameterization of heat transfer based on remote sensing data, and the Surface Energy Balanc...
Turbulence data and wind, temperature profile data are used to analyze turbulence structure within a...
The aerodynamic roughness length (z0m) is a crucial parameter for reliably simulating turbulent exch...
Roughness length and zero-plane displacement over boreal, cool- and warm-temperate forests were obse...
Aerodynamic roughness length z(om) is an important parameter for reliably simulating surface fluxes....
Aerodynamic roughness length (z(om)) is an important parameter for reliably simulating surface fluxe...
Aerodynamic roughness length (z(0)) is one of the main parameters for describing aerodynamic charact...
The estimation of the surface roughness parameters and the choice of the non-dimensional gradient fu...
Aerodynamic roughness length (z(0m)) is a key factor in surface flux estimations with remote sensing...
Three-dimensional velocity components and temperature were measured using the new three-dimensional ...
Information of temporal and spatial variation of aerodynamic roughness length is required in most la...
Three velocity components and temperature were measured using three-dimensional sonic anemometers/th...
Roughness length and zero-plane displacement over three typical surfaces were calculated iteratively...
Aerodynamic roughness height (Zom) is a key parameter required in several land surface hydrological ...
The displacement height d and roughness length z0 are parameters of the logarithmic wind profile and...
<p>The parameterization of heat transfer based on remote sensing data, and the Surface Energy Balanc...
Turbulence data and wind, temperature profile data are used to analyze turbulence structure within a...
The aerodynamic roughness length (z0m) is a crucial parameter for reliably simulating turbulent exch...
Roughness length and zero-plane displacement over boreal, cool- and warm-temperate forests were obse...
Aerodynamic roughness length z(om) is an important parameter for reliably simulating surface fluxes....
Aerodynamic roughness length (z(om)) is an important parameter for reliably simulating surface fluxe...
Aerodynamic roughness length (z(0)) is one of the main parameters for describing aerodynamic charact...
The estimation of the surface roughness parameters and the choice of the non-dimensional gradient fu...
Aerodynamic roughness length (z(0m)) is a key factor in surface flux estimations with remote sensing...
Three-dimensional velocity components and temperature were measured using the new three-dimensional ...
Information of temporal and spatial variation of aerodynamic roughness length is required in most la...
Three velocity components and temperature were measured using three-dimensional sonic anemometers/th...
Roughness length and zero-plane displacement over three typical surfaces were calculated iteratively...
Aerodynamic roughness height (Zom) is a key parameter required in several land surface hydrological ...
The displacement height d and roughness length z0 are parameters of the logarithmic wind profile and...
<p>The parameterization of heat transfer based on remote sensing data, and the Surface Energy Balanc...