1 / 37

Ozone!

Ozone!. 12 th Brewer Meeting – Aosta, Italy 2009. Introduction to Ozone Measurement. Tom McElroy David Wardle Vladimir Savastiouk. Physical Principles of the Dobson Measurement. Beer’s law 1, 2 Ozone absorption Slant path at 22 km;  , m and sec Rayleigh scattering

katoka
Download Presentation

Ozone!

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Ozone! 12th Brewer Meeting – Aosta, Italy 2009

  2. Introduction to Ozone Measurement Tom McElroy David Wardle Vladimir Savastiouk 13th Biennial Brewer Workshop

  3. Physical Principles of the Dobson Measurement Beer’s law 1, 2 Ozone absorption Slant path at 22 km;  , m and sec Rayleigh scattering Langley plots 1, 2 Single wavelength attenuation expression Dobson observations 1, 2 Performance Testing 13th Biennial Brewer Workshop

  4. Handbook Dobson’s Observer’s Handbook 13th Biennial Brewer Workshop

  5. Beer’s Law 1 Cross-section m2 Total optical depth: m2/molecule * molecules / m2 Lost photons: photons / s 13th Biennial Brewer Workshop

  6. Beer’s Law - 2 13th Biennial Brewer Workshop

  7. Beer’s Law - 3 ‘Phenomenological’ 13th Biennial Brewer Workshop

  8. Ozone Absorption - General 13th Biennial Brewer Workshop

  9. Ozone Cross-sections Spectral regions used for ‘optical’ measurements Huggins and Chappuis Cross-sections as Measured in the Laboratory by the GOME FM. GOME- Global Ozone Monitoring Experiment FM – Flight Model 13th Biennial Brewer Workshop

  10. Ozone Absorption - Dobson The tables show the standard Dobson measurement Wavelengths and the optical depths of a 1-cm ozone path. The idea behind both the Dobson and Brewer measurements is that the absolute extinction on a wavelength pair from other things is similar, but the difference in ozone Absorption is large… 13th Biennial Brewer Workshop

  11. Ozone Absorption – Brewer Wavelengths (The small absorption at 324 nm allowed this intensity to be used as a proxy for wavelengths longer than 325 nm in the original short-wavelength-range Brewer UV scans.) 13th Biennial Brewer Workshop

  12. Single-wavelength attenuation expression - 13th Biennial Brewer Workshop

  13. Langley plot: single-wavelength measurement 13th Biennial Brewer Workshop

  14. Differential Measurements 13th Biennial Brewer Workshop

  15. Langley plot – Short and Long Methods 13th Biennial Brewer Workshop

  16. Dobson Observation 13th Biennial Brewer Workshop

  17. Rayleigh scattering 13th Biennial Brewer Workshop

  18. Slant path at 22 km;  , m and sec() 13th Biennial Brewer Workshop

  19. Fery Spectrometer 13th Biennial Brewer Workshop

  20. Dobson Spectrophotometer 13th Biennial Brewer Workshop

  21. Inside…

  22. Brewer Optics ~ 15 cm To Photomultiplier Housing Entrance Slit 13th Biennial Brewer Workshop

  23. Rectifier Phase The Dobson was one of the first opto-electronic instruments to use phase- sensitive detection to improve signal-to-noise ratio and do a direct difference detection. These tracings illustrate the phase setting adjustment made to synchronize the rectifier with the phase of the optical signal. The test is done with a large signal and high signal-to-noise ratio. 13th Biennial Brewer Workshop

  24. Brewer – SH Test • For efficient operation the slits should be open as much as possible (design 7:8) • Only one slit should pass light at one time • Stepping motor must change positions as fast as possible • It must not oscillate when stopped • A non-resonant waveform is generated • The SH test determines the time constant for the waveform 13th Biennial Brewer Workshop

  25. The Brewer – Run/Stop • The Brewer multiplexes rapidly between multiple slits • Photon counting is inhibited while changing slits so the electronics determines the timing interval • The position of the slit mask must change fast with little oscillation to be accurate • The Run/Stop test compares static measurements with dynamic measurements 13th Biennial Brewer Workshop

  26. Measurement Linearity Dobson • Issue largely avoided • Detection of balance only at range of gains • Optical wedge calibrated using 2-source test • ‘N-tables’ used to translate R-values to logs 13th Biennial Brewer Workshop

  27. Linearity - Brewer • Linearity tested explicitly • 2-source test • Done using the DT test • Run with three slit positions • One has 2 slits open at once • Measure: A, B and A&B • Compare: A+B to A&B • Solve for dt in: A = Ao exp( - Ao dt ) B = Bo exp( - Bo dt ) A + B = (Ao + Bo) exp[ - (Ao + Bo) dt ] 13th Biennial Brewer Workshop

  28. Sun Scans 13th Biennial Brewer Workshop

  29. Brewer Sunscan Ozone 13th Biennial Brewer Workshop

  30. The Brewer – SC Test • The solar spectrum is observed under clear conditions (for stability) • The grating angle is scanned by stepping the drive micrometer • An extreme point in the ozone and SO2 is identified near the nominal calibration step • This step position is the calibration point for the instrument (Note that the step number is a function of slant column ozone amount. Traditionally the cal step is chosen near 700 DU slant column ozone amount.) 13th Biennial Brewer Workshop

  31. Ozone v. Step Number 13th Biennial Brewer Workshop

  32. Brewer Calibration • Using direct regression against airmass • Computer-calculated • Station instruments done by comparison to traveling standard Mauna Loa Observatory 13th Biennial Brewer Workshop

  33. Extraterrestrial Constant Lo analysis From Oxford. 13th Biennial Brewer Workshop

  34. Brewer Langley Plot 13th Biennial Brewer Workshop

  35. The Formula… Ozone = (F – Fo) / (mu * alpha) If the ozone is constant, Ozone * alpha = F / mu – Fo / mu Plot F / mu against 1/ mu The slope is Fo 13th Biennial Brewer Workshop

  36. Inverse plot 13th Biennial Brewer Workshop

  37. The End Eureka, Nunavut February 2006

More Related