analysis of spuv aerosol data for the may 2003 bbc2 campaign piet stammes wouter knap knmi
TRANSCRIPT
![Page 1: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/1.jpg)
Analysis of SPUV aerosol data for the May 2003
BBC2 campaign
Piet StammesWouter Knap
KNMI
![Page 2: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/2.jpg)
The SPUV sunphotometerhas 6 spectral channels: 368 nm501 nm675 nm780 nm871 nm 940 nm (H2O)
These channels are 2-15 nm wide.
![Page 3: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/3.jpg)
Data description
• SPUV data available for all days of May 2003, except 22 May.
• Data are 1-minute values of aerosol optical thickness at 368, 501, 675, 780 and 871 nm.
• AOT spectral dependence is characterized by the Angstrom relation:
AOT () -
![Page 4: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/4.jpg)
Data processing
1. Absolute calibration uses the De Bilt time-series (June 1997- March 2003) and the Jungfraujoch calibration campaign (Aug.-Nov. 2003).
2. Correction for Rayleigh scattering and ozone absorption uses actual data of surface pressure and ozone column.
3. Cloud detection is improved: repeated triplet test.
4. Only days with >2 % cloud-free points for the 501 nm channel are considered.
![Page 5: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/5.jpg)
Percentage cloud-free points
Morning values Afternoon values
NB: - Not many cloud-free days during the flights between 8 and 21 May- Clear period end of the month- More cloud-free points in the morning than in the afternoon.
![Page 6: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/6.jpg)
AOT at 501 nm
Morning averages ± Afternoon averages ±
NB: - lower AOT values until 15-20 May, higher values at end of month- PM data lower than AM data in first half of the month.
![Page 7: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/7.jpg)
Angstrom parameter
Morning averages ± Afternoon averages ±
NB: - lower values until 15-20 May, higher values at end of month- high values of Angstrom parameter at end of the month.- low AOT, large particles in first half of month- high AOT, small particles at end of month
![Page 8: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/8.jpg)
Examples of daily variation in aerosol on three days:
4 May, 8 May and 31 May 2003
![Page 9: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/9.jpg)
Diurnal variation of aerosol on 4 May 2003
AOT at 501 nm Angstrom parameter
![Page 10: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/10.jpg)
Diurnal variation of aerosol on 8 May 2003
AOT at 501 nm Angstrom parameter
![Page 11: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/11.jpg)
Diurnal variation of aerosol on 31 May 2003
AOT at 501 nm Angstrom parameter
Number of channels to fit AOT () to -
varies over the day; this changes .
![Page 12: Analysis of SPUV aerosol data for the May 2003 BBC2 campaign Piet Stammes Wouter Knap KNMI](https://reader034.vdocuments.mx/reader034/viewer/2022042821/56649c7b5503460f9492ecce/html5/thumbnails/12.jpg)
Conclusions
• Aerosol optical thickness can vary strongly over the day, probably due to advection and turbulence.
• The BBC2 days with aircraft data are not well suited for aerosol studies.
• Future work:- Intercomparison with CIMEL aerosol data- Combine with the broadband irradiances at the ground to determine the direct aerosol effect.