Roughness length

Roughness length (${\displaystyle z_{0}}$) is a parameter of some vertical wind profile equations that model the horizontal mean wind speed near the ground. In the log wind profile, it is equivalent to the height at which the wind speed theoretically becomes zero in the absence of wind-slowing obstacles and under neutral conditions. In reality, the wind at this height no longer follows a mathematical logarithm. It is so named because it is typically related to the height of terrain roughness elements (i.e. protrusions from and/or depressions into the surface). For instance, forests tend to have much larger roughness lengths than tundra. The roughness length does not exactly correspond to any physical length. However, it can be considered as a length-scale representation of the roughness of the surface.[1]

A plot of a typical log wind profile under statically neutral conditions. The roughness length plays a part in determining the slope of the line.

Mathematical foundation

The roughness length ${\displaystyle z_{0}}$ appears in the expression for the mean wind speed ${\displaystyle u_{z}}$ near the ground derived using the Monin–Obukhov similarity theory:[2]

${\displaystyle u_{z}={\frac {u_{*}}{\kappa }}\left[\ln \left({\frac {z-d}{z_{0}}}\right)+\psi \left({\frac {z-d-z_{0}}{L}}\right)\right],}$

where

• ${\displaystyle u_{*}}$ is the friction velocity
• ${\displaystyle \kappa }$ is the Von Kármán constant
• ${\displaystyle z}$ is the elevation (as measured from the ground)
• ${\displaystyle d}$ is the elevation of the displacement plane (as measured from the ground), which is an offset that accounts for wind-slowing obstacles such as buildings, trees, or any other structures which impede flow
• ${\displaystyle L}$ is the Monin-Obukhov length (which is defined to be the height at which buoyancy and wind shear are equally effective at creating turbulence)
• ${\displaystyle \psi }$ is a correction factor for stability, with ${\displaystyle \psi =0}$ indicating statically neutral conditions.[2] Conditions are statically neutral when the temperature of the air monotonically increases with elevation.[3]

In the simplest possible case (statically neutral conditions and no wind-slowing obstacles), the mean wind speed simplifies to:

${\displaystyle u_{z}={\frac {u_{*}}{\kappa }}\ln \left({\frac {z}{z_{0}}}\right).}$

This provides a method to calculate the roughness length by measuring the friction velocity and the mean wind velocity (at known elevation) in a given, relatively flat location (under neutral conditions) using an anemometer.[4] Of note is that, in this simplified form, the log wind profile is identical in form to the dimensional law of the wall.

Application

As an approximation, the roughness length is approximately one-tenth of the height of the surface roughness elements. For example, short grass of height 0.01 meters has a roughness length of approximately 0.001 meters. Surfaces are rougher if they have more protrusions. Forests have much larger roughness lengths than tundra, for example. Roughness length is an important concept in urban meteorology as the building of tall structures, such as skyscrapers, has an effect on roughness length and wind patterns.

Terrain description	${\displaystyle z_{0}}$ (m)
Open sea, Fetch at least 5 km	0.0002
Mud flats, snow; no vegetation, no obstacles	0.005
Open flat terrain; grass, few isolated obstacles	0.03
Low crops; occasional large obstacles, x/H > 20	0.10
High crops; scattered obstacles, 15 < x/H < 20	0.25
parkland, bushes; numerous obstacles, x/H ≈ 10	0.5
Regular large obstacle coverage (suburb, forest)	1.0
City centre with high- and low-rise buildings	≥ 2

[5]

Relation to other roughness measures

The roughness length is one of many possible measures of the roughness of a surface. For example, in classical mechanics the coefficient of friction is commonly used to measure the roughness of a surface as it relates to the force exerted on another contacted object. And, in fluid dynamics, hydraulic roughness is a measure of the resistance water experiences when flowing over land or through a channel. All of these measures ultimately derive from frictional forces, which result from irregularities on the surfaces of relevance.

References

1. E. Linacre and B. Geerts. "Roughness length". http://www-das.uwyo.edu/~geerts/cwx/notes/chap14/roughness.html.
2. American Meteorological Society Glossary of Meteorology. "aerodynamic roughness length". https://glossary.ametsoc.org/wiki/Aerodynamic_roughness_length.
3. Stull, Roland. "Static Stability and Atmospheric Soundings". https://www.eoas.ubc.ca/courses/atsc113/flying/met_concepts/03-met_concepts/03b-static-stability/index.html.
4. National Center for Atmospheric Research Earth Observing Laboratory. "Calculation of roughness length and displacement height". https://www.eol.ucar.edu/content/calculation-roughness-length-and-displacement-height.
5. WMO Guide to Meteorological Instruments and Methods of Observation WMO-No. 8 page I.5-13

External links

• Aerodynamic Roughness (Length AMS Glossary)
• Surface Roughness Length
• Roughness
• Roughness (AMS Glossary)

See also

• Von Kármán constant
• Monin-Obukhov length
• Wind profile power laws