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Evaluation of Urban Local-Scale Aerodynamic Parameters: Implications for the Vertical Profile of Wind Speed and for Source Areas
by
Grimmond, Sue
, Barlow, Janet
, Kent, Christoph W.
, Halios, Christos H.
, Lindberg, Fredrik
, Gatey, David
, Kotthaus, Simone
in
Aerodynamic roughness length
/ Aerodynamics
/ Anemometric methods
/ Atmospheric boundary layer
/ Atmospheric Protection/Air Quality Control/Air Pollution
/ Atmospheric Sciences
/ Canopy
/ Displacement
/ Doppler lidar
/ Doppler sonar
/ Earth and Environmental Science
/ Earth Sciences
/ Evaluation
/ Formulae
/ geometry
/ Height
/ High frequency
/ Length
/ Lidar
/ Logarithmic wind-speed profile
/ Lookup tables
/ Meteorologi och atmosfärsvetenskap
/ Meteorology
/ Meteorology and Atmospheric Sciences
/ Morphometric methods
/ Morphometry
/ Naturgeografi
/ Parameters
/ Physical Geography
/ Profiles
/ Research Article
/ Roughness
/ Roughness length
/ Roughness parameters
/ Source area
/ Surface geometry
/ Tables
/ United Kingdom
/ Urban areas
/ Variability
/ Velocity measurement
/ Vertical profiles
/ Wind direction
/ Wind speed
/ Zero-plane displacement
2017
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Evaluation of Urban Local-Scale Aerodynamic Parameters: Implications for the Vertical Profile of Wind Speed and for Source Areas
by
Grimmond, Sue
, Barlow, Janet
, Kent, Christoph W.
, Halios, Christos H.
, Lindberg, Fredrik
, Gatey, David
, Kotthaus, Simone
in
Aerodynamic roughness length
/ Aerodynamics
/ Anemometric methods
/ Atmospheric boundary layer
/ Atmospheric Protection/Air Quality Control/Air Pollution
/ Atmospheric Sciences
/ Canopy
/ Displacement
/ Doppler lidar
/ Doppler sonar
/ Earth and Environmental Science
/ Earth Sciences
/ Evaluation
/ Formulae
/ geometry
/ Height
/ High frequency
/ Length
/ Lidar
/ Logarithmic wind-speed profile
/ Lookup tables
/ Meteorologi och atmosfärsvetenskap
/ Meteorology
/ Meteorology and Atmospheric Sciences
/ Morphometric methods
/ Morphometry
/ Naturgeografi
/ Parameters
/ Physical Geography
/ Profiles
/ Research Article
/ Roughness
/ Roughness length
/ Roughness parameters
/ Source area
/ Surface geometry
/ Tables
/ United Kingdom
/ Urban areas
/ Variability
/ Velocity measurement
/ Vertical profiles
/ Wind direction
/ Wind speed
/ Zero-plane displacement
2017
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Evaluation of Urban Local-Scale Aerodynamic Parameters: Implications for the Vertical Profile of Wind Speed and for Source Areas
by
Grimmond, Sue
, Barlow, Janet
, Kent, Christoph W.
, Halios, Christos H.
, Lindberg, Fredrik
, Gatey, David
, Kotthaus, Simone
in
Aerodynamic roughness length
/ Aerodynamics
/ Anemometric methods
/ Atmospheric boundary layer
/ Atmospheric Protection/Air Quality Control/Air Pollution
/ Atmospheric Sciences
/ Canopy
/ Displacement
/ Doppler lidar
/ Doppler sonar
/ Earth and Environmental Science
/ Earth Sciences
/ Evaluation
/ Formulae
/ geometry
/ Height
/ High frequency
/ Length
/ Lidar
/ Logarithmic wind-speed profile
/ Lookup tables
/ Meteorologi och atmosfärsvetenskap
/ Meteorology
/ Meteorology and Atmospheric Sciences
/ Morphometric methods
/ Morphometry
/ Naturgeografi
/ Parameters
/ Physical Geography
/ Profiles
/ Research Article
/ Roughness
/ Roughness length
/ Roughness parameters
/ Source area
/ Surface geometry
/ Tables
/ United Kingdom
/ Urban areas
/ Variability
/ Velocity measurement
/ Vertical profiles
/ Wind direction
/ Wind speed
/ Zero-plane displacement
2017
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Evaluation of Urban Local-Scale Aerodynamic Parameters: Implications for the Vertical Profile of Wind Speed and for Source Areas
Journal Article
Evaluation of Urban Local-Scale Aerodynamic Parameters: Implications for the Vertical Profile of Wind Speed and for Source Areas
2017
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Overview
Nine methods to determine local-scale aerodynamic roughness length
(
z
0
)
and zero-plane displacement
(
z
d
)
are compared at three sites (within 60 m of each other) in London, UK. Methods include three anemometric (single-level high frequency observations), six morphometric (surface geometry) and one reference-based approach (look-up tables). A footprint model is used with the morphometric methods in an iterative procedure. The results are insensitive to the initial
z
d
and
z
0
estimates. Across the three sites,
z
d
varies between 5 and 45 m depending upon the method used. Morphometric methods that incorporate roughness-element height variability agree better with anemometric methods, indicating
z
d
is consistently greater than the local mean building height. Depending upon method and wind direction,
z
0
varies between 0.1 and 5 m with morphometric
z
0
consistently being 2–3 m larger than the anemometric
z
0
. No morphometric method consistently resembles the anemometric methods. Wind-speed profiles observed with Doppler lidar provide additional data with which to assess the methods. Locally determined roughness parameters are used to extrapolate wind-speed profiles to a height roughly 200 m above the canopy. Wind-speed profiles extrapolated based on morphometric methods that account for roughness-element height variability are most similar to observations. The extent of the modelled source area for measurements varies by up to a factor of three, depending upon the morphometric method used to determine
z
d
and
z
0
.
Publisher
Springer Netherlands,Springer,Springer Nature B.V
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