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GSICS Web Meeting, 17 November 2011
Intersatellite Calibration of Kalpana TIR & WV Channels with AIRS and IASI Hyperspectral Observations Space Applications Centre Indian Space Research Organisation Ahmedabad (INDIA) GSICS Web Meeting, 17 November 2011
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Satellite Sensors and Data Used
Indian Geostationary Satellites Kalpana : VHRR INSAT-3A : VHRR INSAT-3D : Imager (6 Channels – VIS, SWIR, MWIR, WV, TIR1, TIR2) Sounder (18 IR + 1 Vis Channels) Hyperspectral IR Sounders IASI (Metop) 8461 IR-Channels (Morning/Evening Observations) AIRS (Aqua) 2378 IR-Channel (Noon/mid-night Observations) Intercalibration period AIRS: 2010 (Jan, Apr, Jul, Oct) IASI: (Jul-Oct)
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Kalpana Launched in Sep 2002 Positioned at 74°E.
Full disk every 30 minutes VHRR VIS : m WV : m TIR : m Spatial resolution (at nadir) : 2 km for VIS 8 km for WV and TIR channels
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Aqua-AIRS and Metop-IASI spectral coverage with Kalpana SRFs for TIR and WV channels
AIRS: Atmospheric InfraRed Sounder Polar Orbiting Aqua (2002) Channels: (650 cm-1 to 2675 cm-1) (3.74 μm μm) Spectral resolution: /1200 Spatial Resolution: 13.5 Km at Nadir Brightness Temperature AIRS IASI: Infrared Atmospheric Sounding Interferometer Polar Orbiting Metop (2007) Channels: (645 cm-1 to 2760 cm-1) (3.62 μm μm) Spectral resolution: cm-1 at SWIR 0.50 cm-1 at LWIR (resampled at 0.25 cm-1) Spatial Resolution: ~12 km at Nadir IASI
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Methodology Convolved radiance of broadband sensor using ‘n’ number of hyperspectral sounders channels may be computed using: Rconv is convolved broadband radiance, RAIRS is radiance of hyper-spectral sounder, superscript ‘i’ is hyper-spectral channel index, SKalp is the sensor response function of Kalpana channels at the central wavenumber of hyper-spectral channel ‘i’, and ‘n’ is the total number of hyper-spectral channels in broadband sensor’s SRF range. Missing or bad channels are interpolated from nearest 2 channels. Conversion of radiances to brightness temperature by inverting the equivalent Planck’s function: a1 (=1.052K) and a2 (=0.996) are the band correction coefficients and (= cm-1) is central wavenumber for Kalpana TIR channel
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Methodology……. Following steps are used:
Convolution of Kalpana-TIR radiance from AIRS radiances environment uniformity test: StdDev of 3x3 AIRS and 5x5 Kalpana pixels (~50x50 km) < 2K Land/Ocean flag: Use only ocean pixels Clear scene: Tb > 285K Spatial Collocation: < 0.2° (i.e. within one pixel resolution) Temporal collocation: ( | tAIRS - tKalp | < 15 min) Zenith angle collocation : | sec(AIRS) – sec(Kalp) | < 0.01 and AIRS & Kalp < 30°
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Comparison of Kalpana Tb with AIRS Convolved Tb for Thermal IR Channel
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Intercalibration of Kalpana IR and WV Channels with IASI
Data Source: IASI L1C received through Eumetcast at SAC/ISRO in BUFR format Methodology Land/sea mask: Use only ocean pixels Temporal Collocation: 5, 15, 30 Minutes Spatial Collocation: Within IASI IFOV (2x2 pixels) Zenith angle collocation: | sec(AIRS) – sec(Kalp) | < 0.01 IASI & Kalpana < 10° Spatial homogeneity test: Wang et al., JAOT 2009, vol.26, (Std. Dev. of Kalpana Tb within one IASI IFOV) / (mean Tb of IASI FOR) < 0.01 Difference max(Tb) - min(Tb) within IASI IFOV <=3.0K
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ISAI Observation geometry
IFOV 50 km 12 km
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Kalpana IR/WV pixels within ISAI IFOV
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Testing of the Intercalibration Procedure with Meteosat-7 TIR and WV Channels
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Meteosat-7 vs IASI convolved
01 June 2011, 0230 GMT EUMETSAT - GSICS webpage for Meteosat-7 vs IASI intercalibration
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Intercalibration Results for Kalpana TIR and WV Channels (Jul-Oct, 2011)
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Temporal collocation criteria : dt < 5 min
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Kalpana TIR Channel Daytime (morning)
Temporal collocation < 30 minutes Mean StDev = 1.3 K (with AIRS: 0.41K day, 0.33K night Clear sky only Tb > 285K)
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Kalpana TIR Channel Night-time (Evening)
Temporal collocation < 30 minutes Mean StDev = 1.3 K (with AIRS: 0.41K day, 0.33K night Clear sky only Tb > 285K)
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Kalpana WV Channel Daytime (morning)
Temporal collocation < 30 minutes Mean StDev = 0.92 K
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Kalpana WV Channel Night-time (Evening)
Temporal collocation < 30 minutes Mean StDev = 0.96 K
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Conclusions Kalpana TIR Channel intercalibrated with AIRS radiances for 2011 (clear sky conditions) Std. Dev. of differences very small K Bias smaller during daytime with seasonal variations Bias higher during nightime Kalpana TIR and WV channel intercalibration with IASI radiances (all-sky conditions Std. Dev. of differences high (1.3K TIR and 0.9K WV) TIR: bias smaller during daytime with seasonal variations during TIR: higher bias during nighttime WV: lower bias during daytime and higher bias during nighttime
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Thank You
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