Roughness lengths and wind profiles over an urban landscape in Beijing, China and their relationship with surface geometric features have been investigated by utilizing a whole-year Beijing 325-m Meteorological Tower data. Preliminary results show that a clear rough-to-smooth transition can be seen in the velocity profile. In addition, wind directions above 63 m are densely distributed with the prevailing winds coming from northwest and southwest, while those below are strongly disordered. Finally, roughness lengths derived from the lower profiles respond well to local surface characteristics and their fetches are generally within an area of 500-m radius
The wind fields and temperature fields data provided by D files from 14 surface observation stations...
In an attempt to develop an improved model for the wind-speed profile valid for urban boundary layer...
Aerodynamic roughness lengths (z(0)) were determined for an urban area and two rice paddies mixed wi...
The urban atmospheric boundary layer (UABL) is complex due to the heterogeneous under-lying city sur...
The urban atmospheric boundary layer (UABL) is complex due to the heterogeneous underlying city surf...
Urbanization has greatly changed the underlying surface roughness characteristics to a great extent ...
In this paper, the impact of urban surface roughness length z0 parameterization scheme on the atmosp...
Urban roughness lengths are estimated from measurements of u and u* at one level under neutral condi...
In an attempt to develop an improved model for the wind-speed profile valid for urban boundary layer...
Several methods to determine the aerodynamic characteristics of a site through analysis of its surfa...
Air pollution gained special attention with the rapid development in Beijing. In January 2013, Beiji...
We propose a new formulation for the wind-speed profile in the urban boundary layer, which can be vi...
High buildings or architectural complex in urban areas remarkably distort the urban surface wind fie...
It is an obvious problem that few studies are conducted despite accelerated urbanization process and...
Roughness length is a critical parameter for estimation of wind conditions, and it is therefore also...
The wind fields and temperature fields data provided by D files from 14 surface observation stations...
In an attempt to develop an improved model for the wind-speed profile valid for urban boundary layer...
Aerodynamic roughness lengths (z(0)) were determined for an urban area and two rice paddies mixed wi...
The urban atmospheric boundary layer (UABL) is complex due to the heterogeneous under-lying city sur...
The urban atmospheric boundary layer (UABL) is complex due to the heterogeneous underlying city surf...
Urbanization has greatly changed the underlying surface roughness characteristics to a great extent ...
In this paper, the impact of urban surface roughness length z0 parameterization scheme on the atmosp...
Urban roughness lengths are estimated from measurements of u and u* at one level under neutral condi...
In an attempt to develop an improved model for the wind-speed profile valid for urban boundary layer...
Several methods to determine the aerodynamic characteristics of a site through analysis of its surfa...
Air pollution gained special attention with the rapid development in Beijing. In January 2013, Beiji...
We propose a new formulation for the wind-speed profile in the urban boundary layer, which can be vi...
High buildings or architectural complex in urban areas remarkably distort the urban surface wind fie...
It is an obvious problem that few studies are conducted despite accelerated urbanization process and...
Roughness length is a critical parameter for estimation of wind conditions, and it is therefore also...
The wind fields and temperature fields data provided by D files from 14 surface observation stations...
In an attempt to develop an improved model for the wind-speed profile valid for urban boundary layer...
Aerodynamic roughness lengths (z(0)) were determined for an urban area and two rice paddies mixed wi...