MODIS Ocean Color Processing Chuck McClain* Processing Approach Calibration/Validation Gene Feldman* Data Processing & Distribution MODIS Team Meeting/

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Presentation transcript:

MODIS Ocean Color Processing Chuck McClain* Processing Approach Calibration/Validation Gene Feldman* Data Processing & Distribution MODIS Team Meeting/ July 13-15, 2004/Baltimore, MD * NASA/GSFC

MODIS Ocean Processing Reorganization MODIS Ocean Color processing reorganized by NASA HQ to coincide with new MODIS Ocean Science Team selection. -Ocean color to lead the NASA Earth Science Enterprise transition to “discipline processing”, i.e., move from “missions to measurements” processing. Operational ocean color data processing transferred from MODAPS to the Ocean Color Discipline Processing Group on February 1. -SST processing remains at MODAPS until HQ defines an alternative processing structure.

MAIN PROCESSING SYSTEM Data from multiple satellite and instrument types In-situ, ancillary, and other data GSFCDAAC FlexibleProcessing Multiple Missions Multiple Missions Rapid Reprocessing Rapid Reprocessing Parallel Processing Parallel Processing Streams (operational, algorithm & cali- ration testing, eval- uation products) ScienceCommunityInteractive Knowledgable Staff Knowledgable Staff Enabling Activities Enabling Activities (SeaBASS, SeaDAS, Calibration RR, etc.) OCDP Management & Staff OCDP Management & Staff Reconfigurable & Scalable CZCSOCTS SeaWIFS TerraMODIS AquaMODIS NPPVIIRS ScienceCommunityNASA Flight Projects NASA HQ ProgramManagement Ocean Color Discipline Processing System Community Agreed Standards and Protocols In Situ Data DataUsers DATA L1 DATA L1-L3 DATA MCST* * MODIS Characterization Support Team (NASA/GSFC)

MODIS OC Processing Strategy Initial focus on MODIS/Aqua -MODIS/Aqua more stable than MODIS/Terra -MODIS/Aqua overlap with NPP/VIIRS Initial emphasis on calibration & Lwn’s -Large seasonal/regional differences between MODIS/(Terra & Aqua) & SeaWiFS Lwn’s Reduced product set until radiometry verified -Simplify processing for radiometry evaluations -Maintain a baseline consistent with SeaWiFS product suite. Expand product suite later.

MODIS Ocean Color Parameters Previous OC Parameter Set -Normalized water-leaving radiances (7) -Aerosol optical thickness (865 nm) -Atmospheric correction epsilon -Aerosol model numbers (2) -Clear water aerosol correction epsilon -CZCS pigment concentration -Chlorophyll-a concentration (3) -Total pigment concentration -Chlorophyll fluorescence line height -Chlorophyll fluorescence baseline -Chlorophyll fluorescence efficiency -Total suspended matter -Coccolithophore pigment concentration -Detached coccolithophore concentration -Calcite concentration -Diffuse attenuation at 490 nm -Phycoerythobilin concentration -Phycourobilin concentration -Instantaneous PAR -Instantaneous absorbed radiation for fluorescence -Gelbstoff absorption coefficient at 400 nm -Phytoplankton absorption coefficient at 675 nm -Total absorption coefficients (5) -Primary production (2 at Level-4) Current OC “Baseline” Parameter Set -Normalized water-leaving radiances (6) -Aerosol optical thickness -Atmospheric correction epsilon -Ångström exponent -Chlorophyll-a (1) -Diffuse attenuation coefficient at 490 nm -SST (near real-time daytime skin temp.) Same masks & flags as OC products Previous OC Parameter Set 38 (does not include archived ancillary data & quality control fields) Current OC Parameter Suite 12 (does not include archived ancillary data)

Calibration/Validation Approach Apply same cal/val approach as for SeaWiFS Common processing codes Work sensor calibration issues with MCST -Solar and lunar calibration analysis and products, e.g., calibration tables, response-vs-scan (RVS), sensor polarization. Systematically test algorithms using both SeaWiFS & MODIS for comparison -Polarization, BRDF, glint, cloud masking, etc. -Global time series with regional analyses (clear-water, deep-water, coastal, basin-latitude zones)

MODIS OC Calibration Prelaunch Calibration & Characterization: (Santa Barbara Research Center) On-Orbit Solar & Lunar Calibration (MODIS Characterization Support Team) MOBY-based Vicarious Calibration Adjustment (D. Clark and OCDP Group) SeaWiFS-MODIS Regional & Global Comparisons (OCDP Group) In-situ/Satellite Match-up Comparisons (OCDP Group) In Situ Data Collection (MODIS Ocean Team) Prelaunch data reviewed by MCST, OCDP, & MODIS Ocean Team members One set of vicarious gains for entire MODIS/Aqua data record. Time-dependent gain factors.

SeaWiFS Stability Monthly views of the moon at ~ 7° phase angle. Gradual monotonic degradation primarily in NIR bands. Global mean deep water Lwn’s with no trends, i.e., repeating annual cycles

MOBY Vicarous Calibration

MODIS(Aqua)/SeaWiFS Lwn Ratios (N. Pacific): Initial comparison

MODIS/SeaWiFS Comparisons -MODIS polarization correction* Polarization tables found to be phase-shifted with approximately half the correct amplitude -BRDF correction (based on Morel et al., 2002) Developed for Case 1 waters (mostly open ocean) –Not accurate in turbid waters Error in algorithm found recently Testing to continue -Quality mask & flag thresholds Sunglint radiance threshold Cloud mask threshold MODIS polarization tables based on prelaunch characterization table. SeaWiFS essentially polarization insensitive.

MODIS(Aqua)/SeaWiFS Lwn Ratios (N. Pacific): Correct polarization (corrected phase & magnitude) 412 nm atmospheric correction problem at high solar zenith angles?

MODIS/Aqua Reprocessing Completed in May ‘04 (~ 1½ weeks) MCST temporally smoothed calibration tables Phase & magnitude corrected polarization tables Simple BRDF correction OC3 chlorophyll-a algorithm -Similar to SeaWiFS OC4v4 algorithm OCDP Group continues work with MCST to refine on-board lunar & solar calibration analyses.

SeaWiFS & MODIS 4-Day Deep-Water Chlorophyll Images 4 day composites, Summer mg/m^3 SeaWiFS MODIS (Correct polarization phase & amplitude)

SeaWiFS Lw OCDPS Repro4 MODIS/Aqua Lw OCDPS Repro

OCDPS Repro4 OC4 Chlorophyll OCDPS Repro OC3 Chlorophyll SeaWiFSMODIS/Aqua

Additional Sensor Calibration Issues Temporal stability: long-term and seasonal Refine “Response vs. Scan” (RVS) or scan modulation functions Minimize mirror-side calibration differences (image banding) Detector to detector calibration (striping) Analyses to be conducted in collaboration with MCST and science community.

Back Up Slides

OCDP SST SST -enhanced to allow use of Reynolds OI SST as input -detailed intercomparison with MODAPS products performed -exact match demonstrated at Level-2 (given same input SST) required correction of MODAPS code for OISST interpolation error MODAPSODPS – Only remaining issue is Level-3 quality masking MODAPS approach has been analyzed in detail implementation plans TBD