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Bidirectional Reflectance Function in Coastal Waters And its Application to the Validation of the Ocean Color Satellites Alexander Gilerson 1 , Soe Hlaing 1 , Tristan Harmel 1 , Alberto Tonizzo 1 , Robert Arnone 2 , Alan Weidemann 2 , Samir Ahmed 1 1 Optical Remote Sensing Laboratory, City College, New York 2  Naval Research Laboratory, Stennis Space Center
Bidirectional Reflectance Distribution Function ( BRDF )  ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Water Body Above water radiometer
Correction for Bidirectional Reflectance Distribution ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
BRDF-CORRECTION Algorithm
[object Object],[object Object],[object Object],[object Object],Outline
Theoretical Background Fundamental equation which relates Rrs to optical properties  [Morel 2002 et. al] : merges reflection and refraction effects that occur when downward irradiance and upward radiance propagate through the air-water interface  f   relates the magnitude of the irradiance reflectance just below the surface to  IOP Angular Coordinate Convention θ v  ~ Viewing angle θ s   ~  solar Zenith φ  ~ solar-sensor relative azimuth BRDF correction:   Set  f  and  Q  for Sun at zenith and nadir view Rrs ( W,IOP ) _corrected Q= bidirectional function  W  =  wind speed ω   = single back-scattering albedo ω  = b b  /  (  a + b b  )     determined by IOP
Bio-optical model and radiative transfer simulation 1053 sets of Viewing & illumination geometries Viewing angle  (  θ v  )   0 o  ~ 80 o solar Zenith  (  θ s  )   0 o  ~ 80 0 relative azimuth  (  φ  )   0 o  ~ 180 o Wavelength: 412,443, 491, 551, 668 nm Inherent Optical Properties (IOP)  Range of input parameters [Chl] = 1 to 10mg/m 3 C NAP  = 0.01 to 2.5mg/m 3 a CDOM  = 0 to 2m -1 ω  = b b  /  (  a + b b  ) can be directly connected to  Rrs  through modeling 500 sets of IOP Obtain  Rrs ( λ ) & equivalent  ω ( λ ) from 500 sets of IOPs to investigate Rrs –  ω  relatioships for large sets of viewing and illumination geometries. Generated as  random  variables in the prescribe ranges typical for  coastal water  conditions Particle Scattering Phase Function Varied with particle Concentration & Composition Radiative transfer simulations  (Hydrolight)  Remote-sensing Reflectance  Rrs ( λ )
Rrs ( λ ) vs Single back-scattering albedo ( ω ) at various illumination and viewing geometries ,[object Object],[object Object],[object Object],Rrs ~ function( ω )  with [ Gordon 1988, Lee 2002 & Park 2005  ]. coefficients are generated for each set of viewing / illumination geometries as well as for each wavelength. These coefficients are applicable to typical coastal water conditions.
CCNY-BRDF correction algorithm Optimized for typical Case-2 water conditions ω  – single backscattering albedo θ s  – Solar zenith angle θ v  – Viewing zenith angle φ   –  Solar-sensor relative azimuth λ – Wavelengths ,[object Object],[object Object],[object Object],Tabulated   coefficients based on radiative transfer computation Use of third order polynomial parameterization based on radiative transfer computation for large range of optical properties    generalized expression
Statistical Analysis/Comparison of the standard MG (Morel/Gentili) and proposed CCNY Algorithms Based on Simulated Dataset (1/2)   ,[object Object],[object Object],Standard Algorithm CCNY Algorithm y  = 0.93* x  – 8.4e -5  (Standard) y  = 1.00* x  – 8.5e -6  (CCNY) Regression lines AAPD(Standard Algo)=9.5% AAPD(CCNY Algo)=0.6% Dispersion
Statistical Analysis of the Algorithms Based on Simulated Dataset (2/2)  ,[object Object],[object Object],[object Object],[object Object],[object Object],CCNY algorithm Standard algorithm Without correction in %
ASSESSMENT OF BRDF-CORRECTION APPLICATION TO ABOVE-WATER DATA AT  LONG ISLAND SOUND COASTAL OBSERVATORY
[object Object],[object Object],LISCO Multispectral SeaPRISM system as part of  AERONET – Ocean Color network [Zibordi et al., 2006] LISCO Site Characteristics LISCO
Water type: Moderately turbid and very productive  (Aurin et al. 2010) Bathymetry : plateau at 13 m depth Location and Bathymetry LISCO Site Characteristics Depth in meters  (GEBCO data)
LISCO Tower LISCO site Characteristics Platform : Collocated multispectral  SeaPRISM  and hyperspectral  HyperSAS  instrumentations since October 2009 12 meters Retractable Instrument Tower Instrument Panel
SeaPRISM instrument ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],HyperSAS Instrument Data acquisition every 30 minutes for high time resolution time series  LISCO Instrumentation
Instrument Panel Unique Capability of Making Near-Concurrent Water-Leaving Radiance From Different Viewing Geometries ,[object Object],[object Object],[object Object],[object Object],Features of the LISCO site SeaPRISM HyperSAS N W
Above Water Signal decomposition Above-Water Data Processing Sun T otal radiance Sky radiance Water leaving radiance Sea surface reflectivity Sun glint radiance E d Rrs =  L w  / E d Down-welling Irradiance Remote-sensing reflectance: Needs to be corrected for the bidirectionality property L i L w θ θ L T   =   L w  +  ρ (W) L i   +  L g   L i
Comparison of SeaPRISM and HyperSAS ,[object Object],[object Object],For all the viewing geometries Both instrument pointing same direction (within  ±10° in Azimuth) Rrs SeaPRISM [sr -1 ] Rrs SeaPRISM [sr -1 ] Rrs HyperSAS [sr -1 ] Rrs HyperSAS [sr -1 ]
Comparison between the Standard MG and Proposed CCNY Algorithm with the LISCO Dataset ,[object Object],[object Object],Before BRDF Correction Corrected with MG Corrected with CCNY
APPLICATION TO OCEAN COLOR MODIS IMAGERY
Satellite Validation Satellite Pixel Selection for Matchup Comparison 3km×3km pixel box for  matchup comparison Exclusion  of pixel box if presence of  cloud-contaminated  pixels in this 9km×9km pixel box  Validation of  MODIS-Aqua  against the  LISCO  Data Satellite Data Processing: Standard NASA Ocean Color Reprocessing 2009 Also exclusion of any pixel flagged by the NASA data quality check processing (Atmospheric correction failure, sun glint contamination,…)
Rrs Time series for the match-up comparison Comparison between LISCO and MODIS Ocean Color data    Qualitative consistency in variations is observed between the in-situ and satellite data. How will the Satellite / in situ data comparison be improved by application of the CCNY BRDF-correction ?
Application to the Satellite Data ,[object Object],[object Object],[object Object],Corrected with Standard Algo Corrected with CCNY AAPD (%) Wavelength (nm) 412 443 491 551 667 Standard 46.43 38.85 16.68 13.61 24.54 CCNY 42.40 34.16 14.93 10.99 21.89 Improvement 4.03 4.69 1.75 2.62 2.65
Conclusions ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
ACKNOWLEDGMENTS NASA AERONET team for SeaPRISM calibration, data processing and support of the site operations  NASA Ocean Color Processing Group for satellite imagery Partial support from: Office of Naval Research (ONR) National Oceanographic and Atmospheric Administration (NOAA)

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MO3.T10.5Ahmed.ppt

  • 1. Bidirectional Reflectance Function in Coastal Waters And its Application to the Validation of the Ocean Color Satellites Alexander Gilerson 1 , Soe Hlaing 1 , Tristan Harmel 1 , Alberto Tonizzo 1 , Robert Arnone 2 , Alan Weidemann 2 , Samir Ahmed 1 1 Optical Remote Sensing Laboratory, City College, New York 2 Naval Research Laboratory, Stennis Space Center
  • 2.
  • 3.
  • 5.
  • 6. Theoretical Background Fundamental equation which relates Rrs to optical properties [Morel 2002 et. al] : merges reflection and refraction effects that occur when downward irradiance and upward radiance propagate through the air-water interface f relates the magnitude of the irradiance reflectance just below the surface to IOP Angular Coordinate Convention θ v ~ Viewing angle θ s ~ solar Zenith φ ~ solar-sensor relative azimuth BRDF correction: Set f and Q for Sun at zenith and nadir view Rrs ( W,IOP ) _corrected Q= bidirectional function W = wind speed ω = single back-scattering albedo ω = b b / ( a + b b )  determined by IOP
  • 7. Bio-optical model and radiative transfer simulation 1053 sets of Viewing & illumination geometries Viewing angle ( θ v ) 0 o ~ 80 o solar Zenith ( θ s ) 0 o ~ 80 0 relative azimuth ( φ ) 0 o ~ 180 o Wavelength: 412,443, 491, 551, 668 nm Inherent Optical Properties (IOP) Range of input parameters [Chl] = 1 to 10mg/m 3 C NAP = 0.01 to 2.5mg/m 3 a CDOM = 0 to 2m -1 ω = b b / ( a + b b ) can be directly connected to Rrs through modeling 500 sets of IOP Obtain Rrs ( λ ) & equivalent ω ( λ ) from 500 sets of IOPs to investigate Rrs – ω relatioships for large sets of viewing and illumination geometries. Generated as random variables in the prescribe ranges typical for coastal water conditions Particle Scattering Phase Function Varied with particle Concentration & Composition Radiative transfer simulations (Hydrolight) Remote-sensing Reflectance Rrs ( λ )
  • 8.
  • 9.
  • 10.
  • 11.
  • 12. ASSESSMENT OF BRDF-CORRECTION APPLICATION TO ABOVE-WATER DATA AT LONG ISLAND SOUND COASTAL OBSERVATORY
  • 13.
  • 14. Water type: Moderately turbid and very productive (Aurin et al. 2010) Bathymetry : plateau at 13 m depth Location and Bathymetry LISCO Site Characteristics Depth in meters (GEBCO data)
  • 15. LISCO Tower LISCO site Characteristics Platform : Collocated multispectral SeaPRISM and hyperspectral HyperSAS instrumentations since October 2009 12 meters Retractable Instrument Tower Instrument Panel
  • 16.
  • 17.
  • 18. Above Water Signal decomposition Above-Water Data Processing Sun T otal radiance Sky radiance Water leaving radiance Sea surface reflectivity Sun glint radiance E d Rrs = L w / E d Down-welling Irradiance Remote-sensing reflectance: Needs to be corrected for the bidirectionality property L i L w θ θ L T = L w + ρ (W) L i + L g L i
  • 19.
  • 20.
  • 21. APPLICATION TO OCEAN COLOR MODIS IMAGERY
  • 22. Satellite Validation Satellite Pixel Selection for Matchup Comparison 3km×3km pixel box for matchup comparison Exclusion of pixel box if presence of cloud-contaminated pixels in this 9km×9km pixel box Validation of MODIS-Aqua against the LISCO Data Satellite Data Processing: Standard NASA Ocean Color Reprocessing 2009 Also exclusion of any pixel flagged by the NASA data quality check processing (Atmospheric correction failure, sun glint contamination,…)
  • 23. Rrs Time series for the match-up comparison Comparison between LISCO and MODIS Ocean Color data  Qualitative consistency in variations is observed between the in-situ and satellite data. How will the Satellite / in situ data comparison be improved by application of the CCNY BRDF-correction ?
  • 24.
  • 25.
  • 26. ACKNOWLEDGMENTS NASA AERONET team for SeaPRISM calibration, data processing and support of the site operations NASA Ocean Color Processing Group for satellite imagery Partial support from: Office of Naval Research (ONR) National Oceanographic and Atmospheric Administration (NOAA)