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Ground-based measurements of tropospheric NO 2 - Comparison of MAX-DOAS results to other instruments for DANDELIONS-. Folkard Wittrock, Hilke Oetjen, Anja Schönhardt, Andreas Richter, John P. Burrows - IUP Bremen Hester Volten, Daan Swart - RIVM Ellen Brinksma - KNMI. Outline.
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Ground-based measurements of tropospheric NO2 - Comparison of MAX-DOAS results to other instruments for DANDELIONS- Folkard Wittrock, Hilke Oetjen, Anja Schönhardt, Andreas Richter, John P. Burrows - IUP Bremen Hester Volten, Daan Swart - RIVM Ellen Brinksma - KNMI
Outline • DANDELIONS campaign • MAX-DOAS • Profile Retrieval Algorithm „BREAM“ • Results – focusing on 2nd campaign in 2006 • BREAM / geometric approach • BREAM / in situ • BREAM / LIDAR • BREAM / satellite • Conclusions and Outlook
DANDELIONS “Dutch Aerosol and Nitrogen Dioxide Experiments for vaLIdation of OMI and SCIAMACHY“ CESAR site (Cabauw) located at 51.971°N, 4.927°E 0.70 m below ASL Dandelions Objectives: Validation of satellite measurements Intercomparison of instruments (NO2, O3, aerosols) NO2: ground in situ, lower tropospheric profile (lidar), total columns MAX-DOAS intercomparison -> ideal for evaluation of MAX-DOAScapabilities for profile retrieval
MAX-DOAS Detection: • UV/vis measurement of scattered sunlight measured for different lines of sight • Method: Differential Optical Absorption Spectroscopy - DOAS • Result: averaged absorption along all contributing light paths -> Slant Column Retrieval: • Correction for vertical sensitivity (airmass factors) depending on several meteorological parameters (e.g. albedo, aerosol) • Optimal Estimation for profile retrieval from ground (BREAM) Results: • VC and profile information for the lower troposphere
Multi Axis (MAX)-DOAS Zenith: Stratosphere O3 NO2 BrO IO OClO IO NO2 H2O BrO HCHO O3 CHOCHO Horizon: Troposphere
MAX-DOAS during Dandelions 2006 – Some Technical Details • The Bremen DOAS instruments: • Spectrometer (f=275mm) for visible Wavelength range: 399.5 – 715.0 nm • Spectrometer (f=500mm) for UV Wavelength range: 324.0 – 409.0 nm • One fixed azimuthal viewing direction: N The telescope on the roof of the portocabin E W • 11 Lines of sight: • Zenith • Scan from 0° to 16° in 2° steps • 30° elevation • Integration time: 1 min • Full scan duration: 12 min or5 scans per hour 54° S
- problems with instruments Dandelions 2006 – NO2 sequence Sat Sun
Dandelions 2006 – NO2 sequence Sat Sun
Bremian Advanced MAX-DOAS Retrieval Algorithm - BREAM Flowchart for BREAM
Bremian Advanced MAX-DOAS Retrieval Algorithm - BREAM • Example of input data and results for BREAM • usually 1 hour temporal steps comprising 3 to 5 scans • retrieval grid 50 m • for NO2 two wavelength regions are used to benefit from different effective light paths
Dandelions 2006 – NO2 in the UV and vis Zenith • Scans show smaller NO2 values for the UV • due to different air mass factors (effective light paths) -> valuable information for profile retrieval scans Wavelength ranges: Vis: 450-497 nm UV: 345-365 nm
Bremian Advanced MAX-DOAS Retrieval Algorithm - BREAM • Averaging Kernel Matrix: • Only one scan • for SZA about 35° • trace of A (number of pieces of independent information): 2.8 • illustrates the high sensitivity to the lowermost layers while for altitudes more than one kilometre there is only very little height information
Bremian Advanced MAX-DOAS Retrieval Algorithm - BREAM Influence of some important input parameters on the retrieved profile (sensitivity study for one day) <-> small effect on derived tropospheric column, reflecting the fact that some parameter errors have different effects at different altitudes (e.g. aerosol)
Conclusions and Outlook • MAX-DOAS NO2 profile and tropospheric column data for almost all golden days • Tropospheric vertical column agrees well with pure geometric approach <-> in agreement with previous studies:VC is not very sensitive to retrieval parameters • Comparison to in situ measurements contradictory: general variation captured well, in particular for polluted days in situ much higher <-> interference problem?? • Comparison with NO2-LIDAR much better in terms of absolute values, but profile shape of the LIDAR is different • All in all not very surprising: NO2 is very variable in time, in space (and in experiment) <-> in particular more profile measurements needed