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Instantaneous Observation of Surface Transmission

5 th GOES Users Conference: P1.12 Validation of a GOES-R Broadband Shortwave Surface Transmission and TOA Albedo Look-Up-Table method . Fred G. Rose, Istvan Laszlo, Thomas P. Charlock, Qiang Fu. Method: Fu-Liou GOesR Look-Up-Table(FLUGOR LUT)

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Instantaneous Observation of Surface Transmission

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  1. 5th GOES Users Conference: P1.12 Validation of a GOES-R Broadband Shortwave Surface Transmission and TOA Albedo Look-Up-Table method.Fred G. Rose, Istvan Laszlo, Thomas P. Charlock, Qiang Fu • Method: Fu-Liou GOesR Look-Up-Table(FLUGOR LUT) • The Langley Fu-Liou SW code an 18 band 4-stream correlated-k delta-eddington code was run using 35 vertical levels to generate two Look-Up-Talbles (LUT) one for clear-sky another for cloudy-Sky together they form an 11 variable LUT giving outputs of TOA broadband albedo and broadband surface transmission. • FLUGOR LUT Inputs: • f { solar zenith angle, PW, O3, • Surface [ albedo, elevation], • Cloud [ fraction, optical depth, Re or De, height], • Aerosol [tau, ssa] } • FLUGOR LUT Output: • BROADBAND SURFACE TRANSMISSION • BROADBAND TOA ALBEDO • Validation Comparisons: • Five years of instantaneous daily daytime CERES overpass data at 45 sites • Full Fu-Liou radiative transfer code results from CERES CRS Ed2b product using CERES observed fluxes, MODIS based cloud and aerosols. Comparisons at TOA and Surface • Surface data at 45 sites from ARM, BSRN, CMDL, SURFRAD processed in to 15 minute averages taken from CERES/CAVE (Ceres Arm Validation Experiment) website. FLUGOR LUT compared to Full CERES Radiative Transfer CRS Ed2b Product TOA Broadband ALBEDO Surface SW BB Transmission Cloud Cover (Percent) Aerosol Optical Depth Cloud Cover (Percent) Aerosol Optical Depth Cosine ( Solar Zenith Angle) Precipitable Water (cm) Surface Albedo (broadband) Cloud Particle Size <30 Re Water, >30 De Ice Cosine ( Solar Zenith Angle) Precipitable Water (cm) Surface Albedo (broadband) Cloud Particle Size <30 Re Water, >30 De Ice FLUGOR LUT Vs. Surface Based Observations of Surface BB Transmission Instantaneous Observation of Surface Transmission FLUGOR LUT surface transmission scatter, means and standard deviation are very similar to FULL CRS Ed2b radiative transfer results. Standard deviations of instantaneous comparison of FULL RT to Surface Observations dwarf the FLUGOR LUT minus FULL CRS Ed2b Radiative transfer instantaneous differences. Cosine ( Solar Zenith Angle) Precipitable Water (cm) Surface Albedo (broadband) Cloud Particle Size <30 Re Water, >30 De Ice Cloud Cover (Percent) Aerosol Optical Depth Surface Elevation (Meters) FLUGOR(LUT) – Ed2b(Full RT) Sfc Transmission ED2b CRS(full RT) – CAVE(obs) Sfc Transmission Full RT – OBS Sfc Transmission LUT – Full RT Sfc Transmission

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