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QA/QC of Solar spectral UV-measurements: Checking for wavelength shifts and spectral shape deviations with focus on error flagging Harry Slaper, PN den Outer, HAJM Reinen
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Flagging output Shift in two wavelength regions: < 325 nm green 0.1 nm yellow 0.2 nm red > 325 nm green 0.2 nm yellow 0.4 nm red starting wavelength (SZA dependent) GREEN spike error flag: shape error > 10% => 2-fold error at single wavelength=> YELLOW at 305 nm corresponds to 2-3 % CIE-error atmospheric variability during the scan: green is subdivided in INSTABLE (shape>3%) HIGHLY INSTABLE (shape>5%)
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Shift and deconvolution analysis: why? Spectral instruments show variation in slit functions (FWHM 0.3 - 2.5 nm)=>comparing spectra High accuracy wavelength calibration required (wavelength shift of 0.03-0.05nm => 1% change in Effective UV)
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Wavelength Shift Analysis
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Correction for slit function effects Measured spectrum: M( ) Iterative ‘Deconvolution’ technique - start spectrum S 0 ( ) (high resol.) - simulate measurement M s0 ( ); - correct start spectrum: S 1 ( ) = (M( ) / M s0 ( )) S 0 ( ) Repeat steps until: S 9 ( )
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Wavelength shift uncertainties Reproducability error< 0.01 nm (FWHM <= 1 nm) Alignment error0.01-0.02 nm Absolute acccuracy< 0.01 nm (depends on Extra Terrestrial)
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Solar zenith angle (in)depence of wavelength shifts using SHICrivm (spectra from RIVM UV monitoring)
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Shift and deconvolution analysis Enables high accuracy wavelength calibration Facilitates direct comparison of spectral readings from different instruments/sites Enables calculation of Standardized spectral UV-data
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Shift and deconvolution software: SHICrivm wavelength dependent shift standardized spectrum -shift and slit corrected -shift corrected effective UV-determination for several Action Spectra Check on spectral anomalies
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Further application of SHICrivm Determine high resolution quality of ET-spectra (Kitt Peak, Atlas 3) Slit function; FWHM estimates Analysis of requirements regarding over/under sampling Facilitate model/measurement intercomparison
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Analysis of spectral shape errors (spikes, cloud variability) Use ratio of readings at two adjacent wavelengths and compare with expected ratio (SHIC) identify shortest wavelength with reliable readings (SHIC and ratio method) identify spikes and cloud variability
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Data from Blumthaler SUSPEN 1997
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Identification of spikes and spectral shape errors Spectral shape errors by comparing readings at subsequent wavelengths with ‘expected’ratio problem how to distinguish between errors and variability proposal shape error >0.03 instable conditions; >0.05 highly instable; >0.10 YELLOW (spikes flag)
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R = 0.812 mean SD of 1 min readings
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Correlation of shape errors (10%) and pyranometer variability (mean of SD within minutes; SD between 1 minute readings)
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Flagging output Shift in two wavelength regions: < 325 nm green 0.1 nm yellow 0.2 nm red > 325 nm green 0.2 nm yellow 0.4 nm red starting wavelength (SZA dependent) GREEN spike error flag: shape error > 10% => 2-fold error at single wavelength=> YELLOW at 305 nm corresponds to 2-3 % CIE-error atmospheric variability during the scan: green is subdivided in INSTABLE (shape>3%) HIGHLY INSTABLE (shape>5%)
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!SHICrivm version 3.012 10-06-2001; Harry Slaper LSO/RIVM, harry.slaper@RIVM.NL ! Quality check shift and structure ! sh1 refers to average shift over wavelength interval: 300.00 325.00 ! sh2 refers to average shift over wavelength interval: 325.00 390.00 ! start_wave indicates effective UV below lowest wavelength where 5 successive readings ! meet criterium for structural checks: 0.250 ! spike and instability checking above the starting wavelength 1061024 sza: 44.842 shift1 flagging : GREEN 0.016 (nm) shift2 flagging : GREEN 0.030 (nm) spike and instability flag: GREEN INSTABLE 3.04 % start wavelength flag : YELLOW 299.04 (nm) efuv below: 0.49 % last wavelength flag : GREEN 379.50 (nm) efuv above: 1.92 %
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SHIC status Version 2.79 released october 2000; 3.012 now tested; UNIX version tested flagging included; faster (1-2 sec per spectrum) spectral shape checks improved shifts below 300 nm possible further improvement: output control
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Next year activities New release of SHIC december 2001 Application of flagging on subsets of data Use in climatological analysis (calculation of effective UV in standardized way) improvement of algorithm to identify atmospheric variability during the scans (OE) implementation at the database (in collaboration with FMI, Ola Engelsen) uncertainty analysis in relation to FWHM
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