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Mina Kang1, Myoung-Hwan Ahn1, Quintus Kleipool2 and Pepijn Veefkind2

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Presentation on theme: "Mina Kang1, Myoung-Hwan Ahn1, Quintus Kleipool2 and Pepijn Veefkind2"— Presentation transcript:

1 Comparison among Reference Solar Spectra using TROPOMI Solar Measurements
Mina Kang1, Myoung-Hwan Ahn1, Quintus Kleipool2 and Pepijn Veefkind2 Department of Atmospheric Science and Engineering, Ewha Womans University 2 Royal Netherlands Meteorological Institute (KNMI)

2 Outline of the Presentation
TROPOMI Instrument TROPOMI Solar Irradiance Reference Solar Spectra TROPOMI In-Orbit ISRF Comparison among Reference Solar Spectra Some Concluding Remarks

3 UV-Vis-NIR-SWIR nadir viewing pushbroom grating spectrometer
TROPOMI Instrument Successful launch of TROPOMI (TROPospheric Ozone Monitoring Instrument) on board the sentinel 5 precursor TROPOMI UV-Vis-NIR-SWIR nadir viewing pushbroom grating spectrometer Spectral Range nm, nm, nm Spectral Resolution nm Spatial Resolution (Nadir) 7 x 7 km2 Courtesy: ESA, Copernicus

4 TROPOMI Instrument Total Column O3, NO2, CO, SO2, CH4, CH2O, H2O, BrO
Tropospheric column O3, NO2 O3 Profile Aerosol AI, AOD, Aerosol Type Courtesy: ESA, Copernicus

5 TROPOMI Instrument Vicarious Calibration for UV-Vis Satellite
Courtesy: ESA 2017 2018 2019 2020 2021 2022 2023 2024 2025 2026 2027 2028 GEMS TEMPO Sentinel-4 Sentinel-5p Sentinel-5

6 TROPOMI Instrument Vicarious Calibration using GEO and LEO Satellite
After the GEMS is launched, we can utilize the AMI which is korea’s advanced metrological imager. We are evaluating the possibility of calibration of VIS channel of GEMS using detected DCC from IR sensor. As a preliminary test, we compared AHI radiance with convolved tropomi radiances. AHI Radiance (Ch.1; 4.7 μm) Convolved TROPOMI Radiance with AHI SRF

7 TROPOMI Solar Irradiance
TROPOMI Measured Solar Irradiance Solar Irradiance obtained from In-orbit test ( ; only single day) TROPOMI Solar Measurement Ratio of Band 2 & Band 3 Inconsistency between band 2 and band 3

8 TROPOMI Solar Irradiance
TROPOMI Measured Solar Irradiance In-orbit test data ( ) TROPOMI Solar Measurements (SWIR) TROPOMI Solar Measurements (NIR) Spike seen in SWIR Need further quality check

9 Reference Solar Spectra
Currently Available Reference Solar Spectra Spectrum Wavelength range [nm] Spectral resolution [nm] Spectral sampling [nm] Uncertainty [%] References NRLSSI2 1.00 2-4 Coddington et al. (2015) ATLAS 2-4 for nm Thuillier et al. (2004) WHI 0.01 2-4 for nm Woods et al. (2008) KNMI 0.025 <4 for nm Dobber et al. (2006) SAO2010 0.04 < 5 for nm Chance and Kurucz (2010) JPL Toon et al. (2014)

10 Reference Solar Spectra
Reference Solar Spectra of TROPOMI High Resolution Reference Solar Spectra TROPOMI Solar Irradiance KNMI (Dobber et al) SAO2010 (Chane and Kurucz) JPL (Toon et al) Band1: [ nm] Band2: [ nm] Band3: [ nm] Band4: [ nm] Band5: [ nm] Band6: [ nm] Band7: [ nm] Band8: [ nm] KNMI SAO2010 SAO2010 JPL

11 TROPOMI In-Orbit ISRFs
Derive TROPOMI In-Orbit Instrument Spectral Response Function Asymmetric Super-Gaussian analytic function (Beirle et al 2016) is used. 𝑇𝑅𝑂𝑃𝑂𝑀𝐼 𝑆𝑜𝑙𝑎𝑟 𝑀𝑒𝑎𝑠𝑢𝑟𝑒𝑚𝑒𝑛𝑡= 𝑅𝑒𝑓𝑠𝑜𝑙 𝜆 𝝓 𝑨𝑺𝑮,𝝀 𝑑𝜆 𝝓 𝑨𝑺𝑮,𝝀 𝑑𝜆 × 𝑨 𝟎 + 𝑨 𝟏 𝜆− 𝜆 𝑎𝑣𝑔 + 𝑨 𝟐 𝜆− 𝜆 𝑎𝑣𝑔 𝑨 𝟑 𝜆− 𝜆 𝑎𝑣𝑔 3 𝐴𝑆𝐺 𝜆 (𝑥)= 𝒌 2𝝕Γ 1/𝑘 × 𝑒 − 𝑥 𝜛− 𝑎 𝜛 𝑘− 𝒂 𝒌 𝑒 − 𝑥 𝜛+ 𝑎 𝜛 𝑘+ 𝒂 𝒌 TROPOMI Solar Irradiance High Resolution Reference Solar Spectra Derived TROPOMI ISRF Spectral Fitting based on Optimal Estimation Algorithm

12 TROPOMI In-Orbit ISRFs
TROPOMI Instrument Spectral Response Function UV Flat-topped, trapezium-like FWHM: 0.45 to 0.5 nm UVIS Triangular + Gaussian, asymmetric FWHM: 0.45 to 0.65 nm NIR Gaussian with rounded top FWHM: 0.34 to 0.35 nm

13 TROPOMI In-Orbit ISRFs
TROPOMI Instrument Spectral Response Function Stable derivation regardless of reference solar spectrum; KNMI or SAO2010 KNMI SAO2010

14 Comparison among Reference Solar Spectra
TROPOMI Measured Solar Irradiance Compare the band 2 and band 3 irradiances with reference solar spectrum (Dobber et al. 2006) Absolute deviations with reference spectrum Relatively high disagreement in band 3 Ratio of TROPOMI Measurements and KNMI

15 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 1 Irradiance vs. KNMI/SAO2010 Use averaged B1 irradiance ( to nm)

16 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 2 Irradiance vs. KNMI/SAO2010 Use averaged B2 irradiance ( to nm)

17 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 3 Irradiance vs. KNMI/SAO2010 Use averaged B3 irradiance ( to nm)

18 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 4 Irradiance vs. KNMI/SAO2010 Use averaged B4 irradiance ( to )

19 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 5 Irradiance vs. SAO2010/JPL Use averaged B5 irradiance ( to )

20 Comparison among Reference Solar Spectra
Comparison Reference Solar Spectra and TROPOMI Irradiance Band 6 Irradiance vs. SAO2010/JPL Use averaged B6 irradiance ( to )

21 KNMI vs. TROPOMI (B1) SAO2010 vs. TROPOMI (B1) KNMI vs. TROPOMI (B2)
Band 1 Y = 1.011x+0.008 R = 0.999 Band 2 Y = 1.171x-0.003 R = 0.996 KNMI vs. TROPOMI (B1) SAO2010 vs. TROPOMI (B1) Band 2 Y = 0.982x+0.016 R = 0.997 Y = 1.042x-0.027 R = 0.996 KNMI vs. TROPOMI (B2) SAO2010 vs. TROPOMI (B2) ( to )

22 SAO2010 vs. TROPOMI (B3) KNMI vs. TROPOMI (B3) KNMI vs. TROPOMI (B4)
Band 3 Y = 0.960x+0.112 R = 0.992 Y = 0.972x+0.122 R = 0.994 SAO2010 vs. TROPOMI (B3) KNMI vs. TROPOMI (B3) Band 4 Y = 1.018x+0.014 R = 0.998 Y = 1.023x-0.071 R = 0.999 KNMI vs. TROPOMI (B4) SAO2010 vs. TROPOMI (B4) ( to )

23 SAO2010 vs. TROPOMI (B5) JPL vs. TROPOMI (B5) SAO2010 vs. TROPOMI (B6)
Band 5 Y = 0.907x+0.575 R = 0.961 Band 5 Y = 0.990x+0.133 R = 0.994 SAO2010 vs. TROPOMI (B6) JPL vs. TROPOMI (B6) Band 6 Y = 1.022x-0.017 R = 0.988 Band 6 Y = 1.001x+0.061 R = 0.997

24 Comparison among Reference Solar Spectra
TK: TROPOMI vs. KNMI TS: TROPOMI vs. SAO2010 SK: SAO2010 vs. KNMI TJ : TROPOMI vs. JPL JS : JPL vs. SAO2010 Comparison Reference Solar Spectra and TROPOMI Irradiance Averaged ratio and differences indicates that TROPOMI measurements show good quality. still preliminary and issues have been identified that will be corrected at the end of the commissioning phase. Band1 [ nm] Band2: [ nm] Band3: [ nm] Band4: [ nm] Band5: [ nm] Band6: [ nm] Ratio Difference [%] Spectrum TK TS SK TJ JS Band 1 0.967 0.849 1.140 -3.311 -15.05 13.99 Band 4 0.987 0.979 1.001 -1.252 -2.118 1.009 Band 2 0.997 0.978 1.020 -0.304 -2.168 2.012 Band 5 0.984 0.995 -2.107 -1.596 -0.519 Band 3 0.972 0.956 1.018 -2.772 -4.448 1.772 Band 6 0.982 1.002 -1.799 -2.024 0.230 ( to )

25 Concluding Remarks TROPOMI successfully launched onboard the Sentinel 5 precursor S5p and S5 are expected to be a good reference for GEMS/TEMPO/S4 Current available reference solar spectra have been compared using TROPOMI preliminary solar measurement Although already of good quality, a few issues regrading the TROPOMI irradiance data to be identified and corrected with the Level 1b algorithm update

26 Acknowledgement The presented work has been performed in the frame of the Sentinel 5P Calibration & Validation (S5P CalVal) Project. Results are based on the use of S-5P in-flight data still subject to in-depth validation activities prior to final release.

27 Thank you :D

28 Reference Solar Spectra
Reference Solar Spectra of TROPOMI Spectral Range [nm] Description Accuracy UV-VIS-NIR nm Dobber et al (2006) [Spectral Resolution nm] [Spectral Sampling 0.01 nm] 4-5 % nm Chance and Kurucz (2010) [Spectral Resolution 0.04 nm] 5 % SWIR nm Thuiller et al (2004) 2 % nm 2%

29

30 Spectral Resolution [nm] Spectral Sampling [nm]
Spectrometer UV UVIS NIR SWIR Band ID 1 2 3 4 5 6 7 8 Spectral Range [nm] Spectral Resolution [nm] 0.5 0.55 0.25 0.23 Spectral Sampling [nm] 0.06 0.2 0.1 <0.1 Spatial Sampling [km2] 21x28 7x7 7x1.8 SNR 100 1500 500

31 Current References SAO2010 vs. KNMI reference spectrum
There are noticeable differences between the two at TEMPO/GEMS resolution (FWHM = 0.6 nm) % differences with 0.6 nm FWHM Gaussian SRF When we compare these spectra at tempo and gems resolution, there are non negligible differences the two. the differences between spectra can show larger variations locally. Especially, in short wavelength range the differences btw two is up to 8 %. SAO 2010 KNMI -- --- Convolved KNMI Convolved SAO Comparison between SAO2010 and KNMI at initial resolution and lower resolution (FWHM= 0.6 nm) Differences between SAO2010 and KNMI (FWHM= 0.6 nm)

32 Current References SAO2010 vs. KNMI reference spectrum
Composite spectrum from different data sources SAO2010 is not absolutely calibrated! Differences between sao2010 and KNMI spectrum are mainly caused by using of the different data sources. SAO2010 is composite spectrum based on hall and Anderson and kurucz 2005. Kurucz 2005 is updated version of kurucz 1984, it is additionally applied atmospheric correction. It means that while sao2010 is updated version of sao96, but it is only updated kittpeak data not absolutely calibrated. On the other hand, KNMI is based on SAO96, but is applied additional radiometric calibration with low resolution spectra (SUSIM and Balloon measurement) Wavelength range/sampling ratio/resolution (FWHM)


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