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Risn Commane, Cdric Floquet,

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Sparse tropical boundary layer and free tropospheric ... Volta. B226. 05/08/06. 2. 2. Independence Day. B225. 03/08/06. 2. 2. Yorkshire Day B. B224 B ... – PowerPoint PPT presentation

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Title: Risn Commane, Cdric Floquet,


1
Aircraft Measurements of OH HO2 in the
Troposphere
  • Róisín Commane, Cédric Floquet,
  • Trevor Ingham, Dwayne Heard, Mat Evans
  • School of Chemistry
  • University of Leeds

2
Hydroxyl Radical (OH)
  • Primary oxidant in troposphere
  • Vital to the breakdown of pollution
  • Methane highest concentration trace gas in
    atmosphere

Estimate 80 global CH4 removed in tropics
(CH4 OH) Fast OH HO2 (HOx)
3
Global OH Measurements
  • Sparse tropical boundary layer and free
    tropospheric measurements of HOx
  • Max HOx production expected in Tropical Summer

Horizontal Lines Fixed Sites Hatched areas
Airborne Measurements
4
HOx Tropospheric Measurements Requirements
  • OH Difficult to Measure
  • Low concentration ( 106 molecule cm-3 0.04
    ppt)
  • Very short lifetime in atmosphere (lt 1 s)
  • Reacts quickly with surfaces
  • Measurement Technique Requirements
  • Highly Sensitive AND Selective
  • Fast Time Resolution (ideally lt 1 min)
  • In situ (aircraft ideal)

5
FAGE Fluorescence Assay by Gas Expansion
A2?

?? 0
  • On-resonance laser-induced fluorescence
  • at low pressure
  • High repetition laser (5 kHz).

Laser beam l308 nm
Fluorescence l308 nm
M
X2?i
?? 0
  • Low pressure (1-2 Torr)
  • reduces
  • Conc. of interfering species
  • Collisional quenching of OH
  • OH Fluorescence longer
  • than laser pulse/
  • other scattering

6
Leeds Air FAGE on the BAe-146during AMMA SOP-2
7
Limitations during AMMA
  • Laser Instability
  • Temperature dependence (YAG unstable gt 36o C)
  • Laser Wavelength Pressure dependence
  • No profile measurements
  • Stepper Motor (Failed sporadically)
  • Lessons Learned
  • Laser requires stable temperatures lower than 34o
    C
  • High moisture conditions (with air conditioning)
    cause condensation on optics in the laser cavity

8
Aircraft FAGE Data AMMA Flight Coverage
OH 7 flights over 6 days HO2 13 flights
over 11 days Typical OH 30 s integration Limit
of Detection (LOD) 7.2 x 105 molecule cm-3 at
1100 m Typical HO2 1 s integration LOD 3.1 x
106 molecule cm-3 at 1100 m.
9
Measurement CycleReference Cell, Laser Power,
Cell Pressure
10
OH and HO2 Online and Offline Raw Signal
11
OH Time Integrated Datashowing associated limits
of detection
12
HO2 Time Integrated Datashowing associated
limits of detection(LOD on separate scale)
13
Interesting Features
  • B228 Large variation observed in OH and HO2
    concentrations during the flight
  • B229 OH and HO2 response to peak in isoprene
  • B235A and B235B Day Vs Night
  • OH below Limit of Detection
  • HO2 still observed into the night
  • B235A HO2 Uptake on water droplets?

14
OH and HO2 concentrations observed during B228OH
ranges from 5 x 106 to lt 6 x 105 molecule cm-3
(LOD)HO2 2.9 x 107 9 x 108 molecule cm-3
15
B229 HO2 Peak coincides with Isoprene Peak. OH
rise observed after
B229
Jim Hopkins, York
16
Large Day-Night Variation in OH Night-time OH lt
LOD Large Day-Night Variation in HO2 Night-time
HO2 observed but greatly reduced
B235A B235B
Noon
Sunset
17
Large Variation in HO2 when sampling in and out
of cloud
B235A B235B
In and Above Cloud
Noon
Sunset
18
Reduction in HO2 when sampling in out of cloud
Claire Reeves
19
Data interpretation strategy
What controls HOx and ROx ? Production - O3
? H2O ? J(O1D) vs J Oxygenates Isoprene
O3 Others? Loss - HO2 HO2, OH
NO2 HO2 Cloud drops OHIsoprene What
controls OH? Recycling from HO2? Loss
through VOCs? When does our understanding
fail? High isoprene loadings? Clouds?
20
How does our understanding change? Conceptual
vision
21
What should we expect?
Isoprene depletes OH
22
What should we expect?
Isoprene depletes OH
23
Future Treatment
What is the composition over West Africa? What
are the principal air masses over West
Africa? Use a cluster analysis approach Done
for ITOP Tie it together with the
meteorology Within each airmass type what
are the modes of variability? Principal
components analysis? New
Mat Evans
24
Final Aircraft FAGE Characterisations
  • Completion of Aircraft FAGE calibration
    characterisation (2 weeks)
  • Application of calibration factor to all
    Aircraft FAGE AMMA data (lt1 week)
  • Submission of 1 s Aircraft FAGE data to BADC
  • (mid March)
  • Addition of FAGE data to full Data Merge (?)

25
Potential Papers ?
  • Aircraft FAGE instrumental?
  • OH Control Mechanism?
  • HO2 Uptake on Clouds?
  • Deviations from Model/Measurement agreement?
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