Radiometric consistency assessment of hyperspectral infrared sounders

The radiometric and spectral consistency among the Atmospheric Infrared Sounder (AIRS), the Infrared Atmospheric Sounding Interferometer (IASI), and the Cross-track Infrared Sounder (CrIS) is fundamental for the creation of long-term infrared (IR) hyperspectral radiance benchmark data sets for both...

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Main Authors: L. Wang, Y. Han, X. Jin, Y. Chen, D. A. Tremblay
Format: Article
Language:English
Published: Copernicus Publications 2015-11-01
Series:Atmospheric Measurement Techniques
Online Access:http://www.atmos-meas-tech.net/8/4831/2015/amt-8-4831-2015.pdf
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author L. Wang
Y. Han
X. Jin
Y. Chen
D. A. Tremblay
author_facet L. Wang
Y. Han
X. Jin
Y. Chen
D. A. Tremblay
author_sort L. Wang
collection DOAJ
description The radiometric and spectral consistency among the Atmospheric Infrared Sounder (AIRS), the Infrared Atmospheric Sounding Interferometer (IASI), and the Cross-track Infrared Sounder (CrIS) is fundamental for the creation of long-term infrared (IR) hyperspectral radiance benchmark data sets for both intercalibration and climate-related studies. In this study, the CrIS radiance measurements on Suomi National Polar-orbiting Partnership (SNPP) satellite are directly compared with IASI on MetOp-A and MetOp-B at the finest spectral scale and with AIRS on Aqua in 25 selected spectral regions through simultaneous nadir overpass (SNO) observations in 2013, to evaluate radiometric consistency of these four hyperspectral IR sounders. The spectra from different sounders are paired together through strict spatial and temporal collocation. The uniform scenes are selected by examining the collocated Visible Infrared Imaging Radiometer Suite (VIIRS) pixels. Their brightness temperature (BT) differences are then calculated by converting the spectra onto common spectral grids. The results indicate that CrIS agrees well with IASI on MetOp-A and IASI on MetOp-B at the long-wave IR (LWIR) and middle-wave IR (MWIR) bands with 0.1–0.2 K differences. There are no apparent scene-dependent patterns for BT differences between CrIS and IASI for individual spectral channels. CrIS and AIRS are compared at the 25 spectral regions for both polar and tropical SNOs. The combined global SNO data sets indicate that the CrIS–AIRS BT differences are less than or around 0.1 K among 21 of 25 spectral regions and they range from 0.15 to 0.21 K in the remaining four spectral regions. CrIS–AIRS BT differences in some comparison spectral regions show weak scene-dependent features.
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spelling doaj.art-f89c9a685a37455ba3544e70db222c742022-12-22T02:43:44ZengCopernicus PublicationsAtmospheric Measurement Techniques1867-13811867-85482015-11-018114831484410.5194/amt-8-4831-2015Radiometric consistency assessment of hyperspectral infrared soundersL. Wang0Y. Han1X. Jin2Y. Chen3D. A. Tremblay4Earth System Science Interdisciplinary Center/Univ. of Maryland, College Park, MD, USANOAA/NESDIS/Center for Satellite Applications and Research, College Park, MD, USAEarth Resources Technology Inc. at NOAA/NESDIS/STAR, Laurel, MD, USAEarth System Science Interdisciplinary Center/Univ. of Maryland, College Park, MD, USAScience Data Processing Inc. at NOAA/NESDIS/STAR, College Park, MD, USAThe radiometric and spectral consistency among the Atmospheric Infrared Sounder (AIRS), the Infrared Atmospheric Sounding Interferometer (IASI), and the Cross-track Infrared Sounder (CrIS) is fundamental for the creation of long-term infrared (IR) hyperspectral radiance benchmark data sets for both intercalibration and climate-related studies. In this study, the CrIS radiance measurements on Suomi National Polar-orbiting Partnership (SNPP) satellite are directly compared with IASI on MetOp-A and MetOp-B at the finest spectral scale and with AIRS on Aqua in 25 selected spectral regions through simultaneous nadir overpass (SNO) observations in 2013, to evaluate radiometric consistency of these four hyperspectral IR sounders. The spectra from different sounders are paired together through strict spatial and temporal collocation. The uniform scenes are selected by examining the collocated Visible Infrared Imaging Radiometer Suite (VIIRS) pixels. Their brightness temperature (BT) differences are then calculated by converting the spectra onto common spectral grids. The results indicate that CrIS agrees well with IASI on MetOp-A and IASI on MetOp-B at the long-wave IR (LWIR) and middle-wave IR (MWIR) bands with 0.1–0.2 K differences. There are no apparent scene-dependent patterns for BT differences between CrIS and IASI for individual spectral channels. CrIS and AIRS are compared at the 25 spectral regions for both polar and tropical SNOs. The combined global SNO data sets indicate that the CrIS–AIRS BT differences are less than or around 0.1 K among 21 of 25 spectral regions and they range from 0.15 to 0.21 K in the remaining four spectral regions. CrIS–AIRS BT differences in some comparison spectral regions show weak scene-dependent features.http://www.atmos-meas-tech.net/8/4831/2015/amt-8-4831-2015.pdf
spellingShingle L. Wang
Y. Han
X. Jin
Y. Chen
D. A. Tremblay
Radiometric consistency assessment of hyperspectral infrared sounders
Atmospheric Measurement Techniques
title Radiometric consistency assessment of hyperspectral infrared sounders
title_full Radiometric consistency assessment of hyperspectral infrared sounders
title_fullStr Radiometric consistency assessment of hyperspectral infrared sounders
title_full_unstemmed Radiometric consistency assessment of hyperspectral infrared sounders
title_short Radiometric consistency assessment of hyperspectral infrared sounders
title_sort radiometric consistency assessment of hyperspectral infrared sounders
url http://www.atmos-meas-tech.net/8/4831/2015/amt-8-4831-2015.pdf
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AT yhan radiometricconsistencyassessmentofhyperspectralinfraredsounders
AT xjin radiometricconsistencyassessmentofhyperspectralinfraredsounders
AT ychen radiometricconsistencyassessmentofhyperspectralinfraredsounders
AT datremblay radiometricconsistencyassessmentofhyperspectralinfraredsounders