Remote Sensing (May 2020)

Field Intercomparison of Radiometer Measurements for Ocean Colour Validation

  • Gavin Tilstone,
  • Giorgio Dall’Olmo,
  • Martin Hieronymi,
  • Kevin Ruddick,
  • Matthew Beck,
  • Martin Ligi,
  • Maycira Costa,
  • Davide D’Alimonte,
  • Vincenzo Vellucci,
  • Dieter Vansteenwegen,
  • Astrid Bracher,
  • Sonja Wiegmann,
  • Joel Kuusk,
  • Viktor Vabson,
  • Ilmar Ansko,
  • Riho Vendt,
  • Craig Donlon,
  • Tânia Casal

DOI
https://doi.org/10.3390/rs12101587
Journal volume & issue
Vol. 12, no. 10
p. 1587

Abstract

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A field intercomparison was conducted at the Acqua Alta Oceanographic Tower (AAOT) in the northern Adriatic Sea, from 9 to 19 July 2018 to assess differences in the accuracy of in- and above-water radiometer measurements used for the validation of ocean colour products. Ten measurement systems were compared. Prior to the intercomparison, the absolute radiometric calibration of all sensors was carried out using the same standards and methods at the same reference laboratory. Measurements were performed under clear sky conditions, relatively low sun zenith angles, moderately low sea state and on the same deployment platform and frame (except in-water systems). The weighted average of five above-water measurements was used as baseline reference for comparisons. For downwelling irradiance ( E d ), there was generally good agreement between sensors with differences of L s k y ) the spectrally averaged difference between optical systems was −2 nm−1 sr−1. For total above-water upwelling radiance ( L t ), the difference was −2 nm−1 sr−1. For remote-sensing reflectance ( R r s ), the differences between above-water TriOS RAMSES were E d accounted for the largest fraction of the variance in R r s , which suggests that minimizing the errors arising from this measurement is the most important variable in reducing the inter-group differences in R r s . The differences may also be due, in part, to using five of the above-water systems as a reference. To avoid this, in situ normalized water-leaving radiance ( L w n ) was therefore compared to AERONET-OC SeaPRiSM L w n as an alternative reference measurement. For the TriOS-RAMSES and Seabird-HyperSAS sensors the differences were similar across the visible spectra with 4.7% and 4.9%, respectively. The difference between SeaPRiSM L w n and two in-water systems at blue, green and red bands was 11.8%. This was partly due to temporal and spatial differences in sampling between the in-water and above-water systems and possibly due to uncertainties in instrument self-shading for one of the in-water measurements.

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