4.4 Article

Characteristics of the Drag Coefficient in the Roughness Sublayer over a Complex Urban Surface

期刊

BOUNDARY-LAYER METEOROLOGY
卷 153, 期 3, 页码 569-580

出版社

SPRINGER
DOI: 10.1007/s10546-014-9949-8

关键词

Atmospheric stability; Drag coefficient; Urban roughness sublayer; Wind speed

资金

  1. State Key Basic Program [2010CB428501]
  2. National Nature Science Foundation of China [40905002]
  3. Jiangsu Provincial Collaborative Innovation Center of Climate Change

向作者/读者索取更多资源

The statistics of momentum exchange in the urban roughness sublayer are investigated. The analysis focuses on the characteristics of the dimensionless friction velocity, , which is defined as the square root of the drag coefficient. The turbulence observations were made at a height of 47 m above the ground on the 325-m meteorological tower, which is located in a very inhomogeneous urban area in Beijing. Under neutral conditions, the dependence of the drag coefficient on wind speed varies with wind direction. When the airflow is from the area of densely built-up buildings, the drag coefficient does not vary with wind speed, while when the airflow is from the area covered by vegetation, the drag coefficient appears to decrease with increasing wind speed. Also, the drag coefficient does not vary monotonically with the atmospheric stability. Both increasing stability and increasing instability lead to the decrease of the drag coefficient, implying that the roughness length and zero-plane displacement may vary in urban areas.

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