the impact of boundary layer dynamics on mixing of pollutants
DESCRIPTION
The impact of boundary layer dynamics on mixing of pollutants. Janet F.Barlow 1 , Tyrone Dunbar 1 , Eiko Nemitz 2 , Curtis Wood 1 , Martin Gallagher 3 , Fay Davies 4 and Roy Harrison 5 1 University of Reading 2 Centre for Ecology and Hydrology 3 University of Manchester - PowerPoint PPT PresentationTRANSCRIPT
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The impact of boundary layer dynamics on mixing of pollutants
Janet F.Barlow1, Tyrone Dunbar1, Eiko Nemitz2, Curtis Wood1, Martin Gallagher3, Fay Davies4 and Roy Harrison5
1University of Reading2Centre for Ecology and Hydrology
3University of Manchester4University of Salford
5 University of Birmingham
Funded by The BOC Foundation
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Urban Boundary Layer dynamics: effect on aerosol distribution
City scale:
(from Oke, 1987)
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Urban Boundary Layer dynamics: effect on aerosol distribution
Neighbourhood scale:
• heat and moisture sources / drag sinks are patchy• aerosol / precursor gas sources are patchy too!• vertical structure of turbulence and aerosols varies spatially and diurnally
Simultaneous measurements required to attribute variability in pollutant concentrations to both dynamical and chemical processes
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REPARTEE campaign 2007
Regents Park
Lidar Site BT TowerDAPPLE roof site
Aim:Intensive observations of aerosols, trace gases and boundary layer dynamics to quantify variability in urban pollutants due to both chemical and meteorological processes.
Special Issue in Atmospheric Chemistry and Physics!
• Collaborators: Birmingham, York, Manchester, Salford (FGAM), Reading, CEH, Lancaster, Leicester, Cambridge, Environment Agency, Bristol
c. 1.6 km
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• Facility for Ground-based Atmospheric Measurement (FGAM) 1.5 micron scanning Doppler lidar (Halo-photonics)
• 24th Oct to 14th Nov 2007 • vertical stare• 30 m resolution gates• integration every 4 sec
• backscatter• along beam Doppler velocity (vertical component)
Doppler lidar measurements
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• R3 sonic anemometers (Gill)• 15th Oct to 15th Nov • 20Hz sampling frequency• height z = 190 m (BT), 17 m (roof)• wind velocity, sonic temperature, fluxes
Sonic anemometers
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Lidar observations – 5th Nov, frontal rain
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Lidar observations – 6th Nov, convective conditions
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Lidar observations – 7th Nov, tracer release day
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Mixing height: all days
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Mixing height: clear days only
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6th Nov: daytime convective BL
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6th: clear night – jet??
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Influence of boundary layer on mixing
• Big changes in: mixing height, strength of turbulence, vertical structure of turbulence
What is the impact on upward mixing of pollutants?
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Estimated time to diffuse from surface up to BT Tower
Tim
e (
secon
ds)
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Conclusions• Doppler lidar gives reliable measurements of turbulent structure of urban boundary layer
• Lidar measurements indicate well-mixed profiles by day, separate layers of aerosol and turbulence at night of depth ~100-500m
Occasionally during night-time ground-level and BT Tower measurements can diverge, i.e. the flow is decoupled from the surface• Mixing timescales depend on boundary layer turbulenceHow far will pollutants be transported vertically (horizontally)?
Latest work: Advanced Climate Technology Urban Laboratory (ACTUAL) Further Doppler lidar measurements in London
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Intercompare BT Tower and lidar
• standard deviation of vertical velocity• big difference during calm, clear night
• across all days, near 1:1 comparison
• across all nights, lidar sometimes less than BT sonic, esp low values
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Intercompare BT Tower and lidar
• BT sonic resampled to 0.25 Hz to match lidar response Lidar sampling rate “too slow” at night to capture small scale turbulence
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Lidar observations – vertical velocity variance
• hourly averages 6th Nov• normalised by convective velocity
where zi=BL depth
w’T’ = heat fluxθ = potential
temp• Compare with Sorbjan (1991), CBL over homogeneous terrain• error bars = standard deviation
Peak below mid-boundary layer, indicating strong shear contribution to mixing
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BT Tower observations
• convective day, positive sensible heat flux, negative at night• clear skies throughout• northerly flow (i.e. from Park)• moderately strong winds
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Intercompare sonic data at rooftop and BT Tower
• Despite statically stable conditions, Rb indicates turbulence still maintained at BT Tower so not completely decoupled
Rb ~ 0.1
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Wind bearing during campaign
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20
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0 45 90 135 180 225 270 315 360
bearing
freq
uenc
y
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Windspeed during campaign
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0 2 4 6 8 10 12 14 16 18
windspeed (m/s)
freq
uenc
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Tracer
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Figure 10: Example of stable conditions (2nd May). a) Mean and standard deviation of sonic temperature,
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29/4/04 0:00 30/4/04 0:00 1/5/04 0:00 2/5/04 0:00 3/5/04 0:00 4/5/04 0:00
time
soni
c te
mpe
ratu
re (
degC
)
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dard
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n so
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T (
deg
C)
BT Ts
Lib Ts
BT sigT
Lib sigT
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Fig 10 b) Ratio of virtual potential temperatures, and normalised turbulent kinetic energy at BT Tower and Lib sites.
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-1
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netic
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rgy
e/U
^2
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ratio
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/roo
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BT e/U2
Lib e/U^2
ThetaBT/ThetaLib
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