Results of the Second SeaWiFS Data Analysis Round Robin, March 2000 (DARR-00)

The accurate determination of upper ocean apparent optical properties (AOPs) is essential for the vicarious calibration of the Sea-viewing Wide Field-of-view Sensor (SeaWiFS) instrument and the validation of the derived data products. To evaluate the importance of data analysis methods upon derived AOP values, the Second Data Analysis Round Robin (DARR-00) activity was planned during the latter half of 1999 and executed during March 2000. The focus of the study was the intercomparison of several standard AOP parameters: (1) the upwelled radiance immediately below the sea surface, L(sub u)(0(-),lambda); (2) the downward irradiance immediately below the sea surface, E(sub d)(0(-),lambda); (3) the diffuse attenuation coefficients from the upwelling radiance and the downward irradiance profiles, L(sub L)(lambda) and K(sub d)(lambda), respectively; (4) the incident solar irradiance immediately above the sea surface, E(sub d)(0(+),lambda); (5) the remote sensing reflectance, R(sub rs)(lambda); (6) the normalized water-leaving radiance, [L(sub W)(lambda)](sub N); (7) the upward irradiance immediately below the sea surface, E(sub u)(0(-)), which is used with the upwelled radiance to derive the nadir Q-factor immediately below the sea surface, Q(sub n)(0(-),lambda); and (8) ancillary parameters like the solar zenith angle, theta, and the total chlorophyll concentration, C(sub Ta), derived from the optical data through statistical algorithms. In the results reported here, different methodologies from three research groups were applied to an identical set of 40 multispectral casts in order to evaluate the degree to which differences in data analysis methods influence AOP estimation, and whether any general improvements can be made. The overall results of DARR-00 are presented in Chapter 1 and the individual methods used by the three groups and their data processors are presented in Chapters 2-4.

[1]  J. Aiken,et al.  The Atlantic Meridional Transect: Spatially Extensive Calibration and Validation of Optical Properties and Remotely Sensed Measurements of Ocean Colour , 1997 .

[2]  C. Mobley,et al.  Estimation of the remote-sensing reflectance from above-surface measurements. , 1999, Applied optics.

[3]  C. McClain,et al.  The calibration and validation of SeaWiFS data , 2000 .

[4]  Prieur,et al.  Analysis of variations in ocean color’ , 2000 .

[5]  M. Kahru,et al.  Ocean Color Chlorophyll Algorithms for SEAWIFS , 1998 .

[6]  William H. Press,et al.  Book-Review - Numerical Recipes in Pascal - the Art of Scientific Computing , 1989 .

[7]  Curtis D. Mobley,et al.  Albedos and Glitter Patterns of a Wind-Roughened Sea Surface , 1986 .

[8]  R. W. Austin,et al.  Ocean Optics Protocols for Satellite Ocean Color Sensor Validation , 2013 .

[9]  Stanford B. Hooker,et al.  Ocean color imaging: CZCS to SeaWIFS , 1993 .

[10]  André Morel,et al.  Light scattering and chlorophyll concentration in case 1 waters: A reexamination , 1998 .

[11]  H. Gordon,et al.  Clear water radiances for atmospheric correction of coastal zone color scanner imagery. , 1981, Applied optics.

[12]  H. Gordon,et al.  Self‐shading of in‐water optical instruments , 1992 .

[13]  S. S. Bruce,et al.  The Fifth SeaWiFS Intercalibration Round-Robin Experiment ( SIRREX-5 ) , July 1996 , 1999 .

[14]  R. W. Austin The remote sensing of spectral radiance from below the ocean surface , 1974 .

[15]  G. Zibordi,et al.  OFFSHORE TOWER SHADING EFFECTS ON IN-WATER OPTICAL MEASUREMENTS , 1999 .

[16]  James W. Brown,et al.  A semianalytic radiance model of ocean color , 1988 .

[17]  S. Maritorena,et al.  An Evaluation of Oceanographic Radiometers and Deployment Methodologies , 2000 .

[18]  L. Prieur,et al.  Analysis of variations in ocean color1 , 1977 .

[19]  G. Zibordi,et al.  Instrument self-shading in underwater optical measurements: experimental data. , 1995, Applied optics.

[20]  E. Fry,et al.  Absorption spectrum (380-700 nm) of pure water. II. Integrating cavity measurements. , 1997, Applied optics.

[21]  S. Hooker An overview of SeaWiFS and ocean color , 1992 .

[22]  S. Hooker,et al.  SeaWiFS Postlaunch Technical Report Series Cumulative Index: Volumes 1-23 , 2003 .

[23]  S. Hooker,et al.  The SeaBOARR-98 Field Campaign , 1999 .

[24]  R. W. Austin,et al.  The Determination of the Diffuse Attenuation Coefficient of Sea Water Using the Coastal Zone Color Scanner , 1981 .

[25]  A. J. Bale,et al.  The Atlantic Meridional Transect: overview and synthesis of data , 2000 .

[26]  Stanford B. Hooker,et al.  Calibration Evaluation and Radiometric Testing of Field Radiometers with the SeaWiFS Quality Monitor (SQM) , 1998 .