Estimating MTF post-launch using lunar imagery – the case of SEVIRI

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Presentation transcript:

Estimating MTF post-launch using lunar imagery – the case of SEVIRI S. Wagner, on behalf of C. Ledez

Procedure – basic concept Step 1 Step 2 Step 3 Step 4

Procedure – basic concept Step 1: Extract the portion of image to be processed One image = One MTF measurement

Procedure – basic concept One image = One MTF measurement Step 2a: derive the edge spread function: Extract all transients - blue curves Estimation of the edge subpixel position (spline interpolation) – red points

Procedure – basic concept One image = One MTF measurement Step 2b: derive the edge spread function: Realignment of the profiles + rescaling of the count levels Truncation after a few Moon pixels (1-3 pixels) Averaging  blue curve

Procedure – basic concept One image = One MTF measurement Step 3: derive the line spread function: Resampling through a fit to have a regular sampling (required for the Fourier transform) + symmetrisation of the fit  red curve Derivative estimate  green curve Adjustments to avoid noisy derivative  underlying red curve  Fourier Transf. = MTF

Procedure – basic concept One image = One MTF measurement

Post-launch characterisation - MTF Some examples - SEVIRI Courtesy C. Ledez - Eumetsat Meteosat-8 SEVIRI HRV MTF North-South

Post-launch characterisation - MTF Results MSG-2 SEVIRI - Channel 01 (VIS 0.6) Courtesy C. Ledez - Eumetsat More images = uncertainties on the MTF measurement Average MTF EW Average MTF NS Nyquist frequency Nyquist frequency

Post-launch characterisation - MTF Results MSG-2 SEVIRI - Channel 02 (VIS 0.8) Courtesy C. Ledez - Eumetsat Average MTF EW Average MTF NS Nyquist frequency Nyquist frequency

Post-launch characterisation - MTF Results MSG-2 SEVIRI - Channel 03 (NIR 1.6) Courtesy C. Ledez - Eumetsat Average MTF EW Average MTF NS Nyquist frequency Nyquist frequency

Known limitations and mitigation – 1/2 Moon ≠ slanted edge selection of ROI on brightest edge E/W or N/S with limited moon edge slope variation estimation of moon shape via polynomial fitting for local edge slope estimation correction of sampling irregularity (e.g. due to pixel position on focal plane) Moon ≠ flat radiance field exclusion of moon image with strong illumination gradient, e.g. crescent estimation of local moon radiance near edge: 1 per radiometric profile EW or NS limitation of profile length inwards: up to edge position + 1 pixel (no limit over deep space)

Known limitations and mitigation – 2/2 Deep space radiance ≠ 0 filtering of stars filtering of ghost image (e.g. AHI) High uncertainty in edge position with aliasing fitting individual radiometric profile with sigmoid / parameters estimated via Kalman type filtering High noise on individual profile merging of all profiles from all detectors, aligned with respect to moon edge position profile averaging via local polynomial smoothing making average profile symmetric visual checking of average profile: no under or over-fitting, good filtering of spurious profiles

Post-launch characterisation - MTF Areas of improvement Proper validation with simulated moon image from HR data planned by EUMETSAT for MTG study of phase dependence effect of craters Moon radiance flat fielding VIS: use of moon radiance model and selenographic coordinates IR: ? MTF estimation at detector level use of swath/detector information

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 01 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 02 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 03 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 04 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 05 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results HIMAWARI-8 AHI - Channel 06 Courtesy C. Ledez - Eumetsat X 23 images = Average MTF EW Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 01 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 02 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 03 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 04 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 05 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Post-launch characterisation - MTF Results GOES-16 ABI - Channel 06 Courtesy C. Ledez - Eumetsat X 1 image = To be compared with: Nyquist frequency

Recommendation - questions MTF curves more useful if provided up to x2 Nyquist  aliasing Can we agree about a frequency range to estimate the MTF? ([0, Nyquist] or [0, 2xNyquist]) What about using a consistent sampling for the MTF? What about agencies sharing the details of their algorithms for estimating MTF post-launch? Do we target a GSICS-recommended approach? What are the next steps for this MTF exercise? Exchange with JMA on the data processing  for the exercise, GIRO imagettes (=“processed” data) were used Exchange with NOAA  was the stretching properly applied? What about