Vicarious calibration of ADEOS-2 GLI visible to shortwave infrared bands using global datasets

We have developed a global vicarious calibration scheme for spaceborne ocean-color sensors, simulating top-of-atmosphere radiance globally using a radiative transfer model, SeaWiFS Level 3 eight-day mean products, and an in-water optical model. This is a relative calibration against two channels used to detect aerosol properties; however, it enables us to determine the spatial and temporal characteristics of the vicarious calibration coefficients (Kvc) without in situ observations. We applied this scheme to the NASDA Global Imager (GLI), which operated from January 25, 2003 to October 24, 2003. Kvc exhibited the following properties: (1) channel characteristics of 1.0-1.1 (GLI was lower than the simulation) in channels 1-9 (380-565 nm), nearly 1.0 in channels 10-19 (625-865 nm), and 0.91-0.98 in channels 24-29 (1050-2210 nm); (2) scan-angle dependency and its temporal changes in channels 1-3; and (3) scan-mirror side differences and temporal changes. Applying Kvc to GLI ocean-color processing produced outputs consistent with the ground observation data. This scheme is also useful for generating consistent products from different ocean-color sensors in orbit.

[1]  T. Eck,et al.  Accuracy assessments of aerosol optical properties retrieved from Aerosol Robotic Network (AERONET) Sun and sky radiance measurements , 2000 .

[2]  Xavier Briottet,et al.  Results of POLDER in-flight calibration , 1999, IEEE Trans. Geosci. Remote. Sens..

[3]  Bryan A. Franz,et al.  Comparing the ocean color measurements between MOS and SeaWiFS: a vicarious intercalibration approach for MOS , 2000, IEEE Trans. Geosci. Remote. Sens..

[4]  R. Evans,et al.  Coastal zone color scanner “system calibration”: A retrospective examination , 1994 .

[5]  Tomohiko Oishi,et al.  Efficient use of an improved radiative transfer code to simulate near-global distributions of satellite-measured radiances. , 2003, Applied optics.

[6]  C. McClain,et al.  Calibration of SeaWiFS. II. Vicarious techniques. , 2001, Applied optics.

[7]  Teruyuki Nakajima,et al.  Matrix formulations for the transfer of solar radiation in a plane-parallel scattering atmosphere. , 1986 .

[8]  Toshiyoshi Kimura,et al.  First results from GLI’s solar calibration , 2003, SPIE Optics + Photonics.

[9]  B. Johnson Coastal Zone Color Scanner , 1988 .

[10]  G. Thuillier,et al.  The Solar Spectral Irradiance from 200 to 2400 nm as Measured by the SOLSPEC Spectrometer from the Atlas and Eureca Missions , 2003 .

[11]  K. Voss,et al.  Validation of atmospheric correction over the oceans , 1997 .

[12]  M. Kishino,et al.  Development of a Neural Network Algorithm for Retrieving Concentrations of Chlorophyll, Suspended Matter and Yellow Substance from Radiance Data of the Ocean Color and Temperature Scanner , 2004 .

[13]  H. Gordon Atmospheric correction of ocean color imagery in the Earth Observing System era , 1997 .

[14]  William L. Barnes,et al.  MODIS on-orbit calibration and characterization , 2003 .

[15]  Charles,et al.  SeaWiFS Postlaunch Calibration and Validation Analyses , Part 1 , 2000 .

[16]  Thomas S. Pagano,et al.  Prelaunch characteristics of the Moderate Resolution Imaging Spectroradiometer (MODIS) on EOS-AM1 , 1998, IEEE Trans. Geosci. Remote. Sens..

[17]  Aisheng Wu,et al.  MODIS reflective solar bands uncertainty analysis , 2004, SPIE Optics + Photonics.

[18]  Robert Frouin,et al.  Early phase analysis of OCTS radiance data for aerosol remote sensing , 1999, IEEE Trans. Geosci. Remote. Sens..

[19]  Kazuhiro Tanaka,et al.  Calibration and instrument status of ADEOS-II Global Imager , 2004, SPIE Remote Sensing.

[20]  Hiroshi Murakami,et al.  Early phase evaluations of GLI vicarious calibration factors for ocean-color channels , 2003, SPIE Optics + Photonics.

[21]  E. Shettle,et al.  Models for the aerosols of the lower atmosphere and the effects of humidity variations on their optical properties , 1979 .

[22]  K. Stamnes,et al.  Numerically stable algorithm for discrete-ordinate-method radiative transfer in multiple scattering and emitting layered media. , 1988, Applied optics.

[23]  T. Nakajima,et al.  Optimization of the Advanced Earth Observing Satellite II Global Imager channels by use of radiative transfer calculations. , 1998, Applied optics.

[24]  Teruyuki Nakajima,et al.  Algorithms for radiative intensity calculations in moderately thick atmospheres using a truncation approximation , 1988 .

[25]  Robert A. Barnes,et al.  SeaWiFS prelaunch radiometric calibration and spectral characterization , 1995 .

[26]  Masahiro Hori,et al.  Vicarious calibration of GLI by ground observation data , 2005, IEEE Transactions on Geoscience and Remote Sensing.

[27]  Howard R. Gordon,et al.  In-Orbit Calibration Strategy for Ocean Color Sensors , 1998 .

[28]  Menghua Wang,et al.  Retrieval of water-leaving radiance and aerosol optical thickness over the oceans with SeaWiFS: a preliminary algorithm. , 1994, Applied optics.

[29]  Robert A. Barnes,et al.  SeaWiFS Technical Report Series. Volume 22: Prelaunch Acceptance Report for the SeaWiFS Radiometer , 1994 .

[30]  Robert Frouin,et al.  Vicarious calibration of the POLDER ocean color spectral bands using in situ measurements , 1999, IEEE Trans. Geosci. Remote. Sens..

[31]  Hiroshi Murakami,et al.  GLI early calibration results for oceanographic applications , 2003, SPIE Optics + Photonics.