Abstract

Ocean colour is recognised as an Essential Climate Variable (ECV) by the Global Climate Observing System (GCOS); and spectrally-resolved water-leaving radiances (or remote-sensing reflectances) in the visible domain, and chlorophyll-a concentration are identified as required ECV products. Time series of the products at the global scale and at high spatial resolution, derived from ocean-colour data, are key to studying the dynamics of phytoplankton at seasonal and inter-annual scales; their role in marine biogeochemistry; the global carbon cycle; the modulation of how phytoplankton distribute solar-induced heat in the upper layers of the ocean; and the response of the marine ecosystem to climate variability and change. However, generating a long time series of these products from ocean-colour data is not a trivial task: algorithms that are best suited for climate studies have to be selected from a number that are available for atmospheric correction of the satellite signal and for retrieval of chlorophyll-a concentration; since satellites have a finite life span, data from multiple sensors have to be merged to create a single time series, and any uncorrected inter-sensor biases could introduce artefacts in the series, e.g., different sensors monitor radiances at different wavebands such that producing a consistent time series of reflectances is not straightforward. Another requirement is that the products have to be validated against in situ observations. Furthermore, the uncertainties in the products have to be quantified, ideally on a pixel-by-pixel basis, to facilitate applications and interpretations that are consistent with the quality of the data. This paper outlines an approach that was adopted for generating an ocean-colour time series for climate studies, using data from the MERIS (MEdium spectral Resolution Imaging Spectrometer) sensor of the European Space Agency; the SeaWiFS (Sea-viewing Wide-Field-of-view Sensor) and MODIS-Aqua (Moderate-resolution Imaging Spectroradiometer-Aqua) sensors from the National Aeronautics and Space Administration (USA); and VIIRS (Visible and Infrared Imaging Radiometer Suite) from the National Oceanic and Atmospheric Administration (USA). The time series now covers the period from late 1997 to end of 2018. To ensure that the products meet, as well as possible, the requirements of the user community, marine-ecosystem modellers, and remote-sensing scientists were consulted at the outset on their immediate and longer-term requirements as well as on their expectations of ocean-colour data for use in climate research. Taking the user requirements into account, a series of objective criteria were established, against which available algorithms for processing ocean-colour data were evaluated and ranked. The algorithms that performed best with respect to the climate user requirements were selected to process data from the satellite sensors. Remote-sensing reflectance data from MODIS-Aqua, MERIS, and VIIRS were band-shifted to match the wavebands of SeaWiFS. Overlapping data were used to correct for mean biases between sensors at every pixel. The remote-sensing reflectance data derived from the sensors were merged, and the selected in-water algorithm was applied to the merged data to generate maps of chlorophyll concentration, inherent optical properties at SeaWiFS wavelengths, and the diffuse attenuation coefficient at 490 nm. The merged products were validated against in situ observations. The uncertainties established on the basis of comparisons with in situ data were combined with an optical classification of the remote-sensing reflectance data using a fuzzy-logic approach, and were used to generate uncertainties (root mean square difference and bias) for each product at each pixel.

Highlights

  • Visible spectral radiometry of the ocean provides time series of digital chlorophyll fields on synoptic scales

  • Pixels considered good are those not flagged as clouds or as sea ice or floating vegetation and where the quality flags provided by the respective atmospheric correction algorithms permitted usage of the retrieved marine reflectance

  • The strategy adopted in OC-climate change initiative (CCI) involves the production of a merged data set of remote-sensing reflectances (Rrs) from the main ocean-colour data streams, currently SeaWiFS, MERIS MODIS-Aqua, and VIIRS, though initial versions did not include VIIRS

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Summary

Introduction

Visible spectral radiometry of the ocean (ocean-colour remote sensing) provides time series of digital chlorophyll fields (a measure of phytoplankton abundance) on synoptic scales. These data have stimulated a revolution in biological oceanography, as well as in Earth System science, and they have enabled many important advances [1]. 1997 to 2018 is the most internally consistent (all radiometric products band-shifted to a common set of bands corresponding to SeaWiFS (Sea-viewing Wide-Field-of-view Sensor)) and stable (corrected for inter-sensor bias) ocean-colour record available so far It is complete with estimates of uncertainty and, thanks to a new procedure for atmospheric correction Expansions & Definitions δ λ μ adg bias correction wavelength median ratio absorption coefficient of detrital particles and coloured dissolved organic matter (or gelbstoff) combined absorption coefficient of phytoplankton total absorption coefficient back-scattering coefficient for particles vertical attenuation coefficient for downwelling irradiance normalised remote-sensing reflectance

User Consultation
Satellite Data
In Situ Data
Match-Up Database
Algorithm Selection Criteria
Objective Scoring System Based on Quantitative and Qualitative Criteria
Quantitative Criteria
Qualitative Criteria
Atmospheric Correction
Pixel Identification
Cloud Screening
Sea-Ice Detection
Mixed-Pixel Identification
Validation of Pixel-Identification Algorithm
Additional Filters and Post-Filters
Band Shifting
Bias Correction and Merging
Generation of Optical Classes
10. In-Water Algorithms
11. Uncertainties
12. Product Generation
13. Validation of Products
14.1. Improved Coverage
14.2. Uncertainty Characterisation Based on Validation
14.3. Merged Radiances that Band Shifted and Bias Corrected
Findings
15. Concluding Remarks
Full Text
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