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

The statistics of momentum exchange in the urban roughness sublayer are investigated. The analysis focuses on the characteristics of the dimensionless friction velocity, $${u_{*}}/U$$u∗/U, 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.

[1]  Timo Vesala,et al.  Intra-City Variation in Urban Morphology and Turbulence Structure in Helsinki, Finland , 2013, Boundary-Layer Meteorology.

[2]  S. Larsen,et al.  On the Determination of the Neutral Drag Coefficient in the Convective Boundary Layer , 1998 .

[3]  J. Finnigan,et al.  A simple unified theory for flow in the canopy and roughness sublayer , 2007 .

[4]  Michael R. Raupach,et al.  Simplified expressions for vegetation roughness length and zero-plane displacement as functions of canopy height and area index , 1994 .

[5]  M. Rotach Simulation Of Urban-Scale Dispersion Using A Lagrangian Stochastic Dispersion Model , 2001 .

[6]  M. Kanda,et al.  Flux-gradient profiles for momentum and heat over an urban surface , 2006 .

[7]  Andreas Christen,et al.  Atmospheric turbulence and surface energy exchange in urban environments : results from the Basel Urban Boundary Layer Experiment (BUBBLE) , 2005 .

[8]  Mathias W. Rotach,et al.  Mean Flow and Turbulence Characteristics in an Urban Roughness Sublayer , 2004 .

[9]  Jianning Sun,et al.  Observational verification of urban surface roughness parameters derived from morphological models , 2008 .

[10]  Ivan Mammarella,et al.  The Effect of Stratification on the Aerodynamic Roughness Length and Displacement Height , 2008 .

[11]  C. Klipp Wind Direction Dependence of Atmospheric Boundary Layer Turbulence Parameters in the Urban Roughness Sublayer , 2007 .

[12]  Christian Feigenwinter,et al.  Vertical Structure of Selected Turbulence Characteristics above an Urban Canopy , 1999 .

[13]  Ian P. Castro,et al.  Near Wall Flow over Urban-like Roughness , 2002 .

[14]  M. Al-Jiboori Correlation Coefficients in Urban Turbulence , 2008 .

[15]  Niels Otto Jensen,et al.  Determination Of The Surface Drag Coefficient , 2001 .

[16]  Kusuma G. Rao,et al.  Estimation of the Exchange Coefficient of Heat During Low Wind Convective Conditions , 2004 .

[17]  M. Roth Turbulent transfer relationships over an urban surface. II: Integral statistics , 1993 .

[18]  T. Oke,et al.  Relative Efficiencies of Turbulent Transfer of Heat, Mass, and Momentum over a Patchy Urban Surface , 1995 .

[19]  Janet F. Barlow,et al.  Turbulent Flow at 190 m Height Above London During 2006–2008: A Climatology and the Applicability of Similarity Theory , 2010 .

[20]  Timothy R. Oke,et al.  Aerodynamic Properties of Urban Areas Derived from Analysis of Surface Form , 1999 .

[21]  I. Mammarella,et al.  The Effect of Stratification on the Aerodynamic Roughness Length , 2009 .

[22]  C. S. B. Grimmond,et al.  Progress in measuring and observing the urban atmosphere , 2006 .

[23]  L. Quan,et al.  Relationship between turbulent flux and variance in the urban canopy , 2009 .

[24]  Ian P. Castro,et al.  Wind-Direction Effects on Urban-Type Flows , 2012, Boundary-Layer Meteorology.

[25]  Matthias Roth,et al.  Review of atmospheric turbulence over cities , 2007 .

[26]  Jianning Sun,et al.  Impact of surface variations on the momentum flux above the urban canopy , 2010 .

[27]  Ian P. Castro,et al.  Turbulence Over Urban-type Roughness: Deductions from Wind-tunnel Measurements , 2006 .

[28]  Hans Bergström,et al.  Turbulence characteristics in a near neutrally stratified urban atmosphere , 1982 .

[29]  M. Raupach Drag and drag partition on rough surfaces , 1992 .

[30]  A. Christen,et al.  The Budget of Turbulent Kinetic Energy in the Urban Roughness Sublayer , 2009 .

[31]  Susumu Oikawa,et al.  Turbulence characteristics and organized motion in a suburban roughness sublayer , 1995 .

[32]  C. Kottmeier,et al.  Internal atmospheric gravity waves near the coast of Antarctica , 1993 .

[33]  Timothy R. Oke,et al.  Flux and turbulence measurements at a densely built‐up site in Marseille: Heat, mass (water and carbon dioxide), and momentum , 2004 .

[34]  Mathias W. Rotach,et al.  Turbulence close to a rough urban surface part II: Variances and gradients , 1993 .

[35]  J. Garratt The Atmospheric Boundary Layer , 1992 .

[36]  Mathias W. Rotach,et al.  Turbulence close to a rough urban surface part I: Reynolds stress , 1993 .

[37]  Hu Fei,et al.  Surface roughness around a 325-m meteorological tower and its effect on urban turbulence , 2005 .

[38]  R. Stull An Introduction to Boundary Layer Meteorology , 1988 .

[39]  I. Harman The Role of Roughness Sublayer Dynamics Within Surface Exchange Schemes , 2011, Boundary-Layer Meteorology.

[40]  Mathias W. Rotach,et al.  A wind tunnel study of organised and turbulent air motions in urban street canyons , 2001 .