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Radiometric inter-comparison of IASI

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Presentation on theme: "Radiometric inter-comparison of IASI"— Presentation transcript:

1 Radiometric inter-comparison of IASI
IASI-A / IASI-B, IASI / AIRS, IASI / CrIS Denis JOUGLET (Successor of Denis Blumstein for the IR sounders inter-calibration) with J. Chinaud, X. Lenot, D. Blumstein, E. Pequignot

2 Introduction Objectives of our inter-comparison study Overview
External validation of the IASI radiometric calibration, complimentary to the performance monitoring done by the IASI TEC Checks the long term data quality, in particular for climatology CNES participation to the GSICS Overview IASI / AIRS inter-comparison Prototyped by D. Blumstein Development of the SIC tool, with industrial development rules Under exploitation in routine mode Still evolving IASI-A / IASI-B inter-comparison Based on the SIC tool with adaptations Will be activated during the IASI-B commissioning phase IASI / CrIS inter-comparison To develop, with SIC as a basis

3 Reminder on IASI, AIRS, CrIS
AIRS/Aqua (since 2002), IASI/Metop-A (since 2006), CrIS/NPP (since 2011), IASI/Metop-B Sun-synchronous polar orbits, local time: 1h30 am/pm, 9h30 am/pm, 1h30 am/pm High resolution TIR spectrometers, designed for atmospheric studies Spectral range : ~ cm-1 ( µm) AIRS (grating) : 2378 channels, 3 separate bands, variable spectral resolution cm-1 IASI (FTS) : 8461 channels, continuous coverage, constant spectral resolution 0.5 cm-1 CrIS (FTS): 1305 channels, 3 separate bands, variable spectral resolution cm-1

4 Status of IASI-A and IASI-B
IASI-A is performing very well after almost 6 years in orbit No redundancy used All mission requirements are met : both instrument and processing The instrument is extremely stable : radiometry, spectral, geometry Mechanisms (Cube Corner, Scan) show no evolution in orbit Radiator (passive cooling) show no evolution in orbit IASI-B Current CAL/VAL planning: METOP-B launch : September 17th 2012 First science data : October 24th 2012 L1 early dissemination (end of phase A) : January 15th 2013 L1 Operational dissemination (end of phase B) : March 12th 2013 End of CAL/VAL (end of phase C) : April 2013

5 IASI / AIRS : methodology 1/2
Work with CNOs (Common Nadir Observations) = Simultaneous Nadir Overpasses with a tolerancy on the time delay between IASI & AIRS up to 20min  Same scene and similar observation conditions  Increase the amount of data: ~ 34 CNOs every 3 days, ~10000 events in 2007 – 2011  always at high latitudes Spatial match: Pixels are not colocated Zonal averaging for IASI and AIRS around the tracks crossing Warning about heterogeneous scenes Geographical location of CNOs

6 IASI / AIRS : methodology 2/2
Spectral match: Work with IASI L1C, AIRS L1B 33 broad pseudo-bands (PBs) = summation of elementary channels (most widths: 23 to 63 cm-1)  Reduces noise and spectral resolution differences  Takes AIRS spurious channels into account through a weighted summation of the IASI channels Other methods under progress similar channels (statistical similar behavior) convolved channels Comparison of ΔT = TIASI - TAIRS in each PB Instrumental functions of one PB for AIRS (including spurious channels), for IASI without weighting in the channels summation and for IASI with weighting

7 IASI / AIRS : some results
SIC operational for systematic download and comparison of data AIRS data from NASA website IASI data from Eumetsat FTP or UMARF Monitoring of calibration with time ΔT = f(date) by PB  IASI and AIRS radiometric calibration are stable and very close  No seasonal or inter-annual trends 1 dot = 1 scene Monthly means

8 IASI / AIRS : some results
2011 Study of biases and st dev  AIRS & IASI radiometric calibration very close (|NeDT| < 0.1K)  Small biases under investigation Dependency of ΔT with Scene temperature (surface or atmo)  larger dispersion at high Tb  Very small trend = small non linearities Dependency of | ΔT | with Scene temperature heterogeneity IASI / AIRS temporal delay 2010 Abs(T(AIRS) – T(IASI))

9 IASI-A / IASI-B : common observations
Metop-B : same orbit as Metop-A with 180° shift  IASI-A & -B have no Simultaneous Nadir Overpasses Relative location of the tracks :  IASI-A & -B have many common observations For each IASI-A line, with the IASI-B previous and following tracks Possible for all latitudes Off-nadir observations (nadir at the poles) 50 min systematic delay between IASI-A and IASI-B

10 IASI-A / IASI-B : selection of scenes
We choose to use these common observations, focusing on: The IASI columns of similar viewing absolute angles (same atmospheric thickness from both obs) = opposite SNs The most relevant regions = homogeneous and stable in 50 min Pre-selection based on: IASI engineering data Differences in IIS/AVHRR A & B temperatures Inter- and intra-pixel IIS/AVHRR homogeneity Oceans Amounts of snow, clouds ECMWF analysis data: NRT processing of T and H fields Daily Δfield, converted in daily Δspectrum through 4AOP jacobians Daily NeDT and ranking “Geophysical” daily NeDT 0.74K 19.92K

11 IASI-A / IASI-B : methodology
Data processing: based on the IASI / AIRS software IASI 1C data from Eumetsat FTP Spatial match: Zonal averaging for IASI-A and IASI-B spectra Spectral match, ΔT comparison: at IASI elementary channel at pseudo-band level  reduces noise and avoids any possible spectral bias An atmosphere correction by double differences will be available if necessary, using meteo profiles Tool development is finished Validated with IASI-B simulated data  Tool ready for cal/val and routine Test of the tool with simulated data

12 IASI / CrIS : under construction
We want to perform the same job for IASI / CrIS Comparison to IASI-A and to IASI-B Method: same as for IASI / AIRS because same orbital configuration Work with zonal averaging ΔT comparison at pseudo-band level ΔT comparison of convolved channels (construction of CrIS-like spectra by convolution from IASI)  Tool under construction CrIS data downloaded from EumetCast Reader for BUFR format Need for CrIS ISRFs Should be ready by october

13 Conclusions Status of the tools:
IASI / AIRS: under exploitation, a publication is to come  Very close cross-calibration, very stable with time IASI-A / IASI-B: the tool is ready for cal/val and routine IASI / CrIS: start of implementation Feel free to come and see my poster! Nr 96 (session 5) Contact for any questions:


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