Abstract

Satellite ocean color remote sensing is the primary method to retrieve synoptic measurements of the optical properties of the ocean on large spatial and regular time scales.Through bio-optical modelling, changes in ocean color spectra can be linked to changes in marine 2 ecosystem and biogeochemical properties. Bio-optical algorithms rely on assumptions about the covariance of marine constituents as well as the relationships among their inherent and apparent optical properties. Validation with in situ measurements of in-water constituents and their optical properties is required to extrapolate local knowledge about ocean color variations to global scales.Here, we evaluate seasonal and spatial relationships between optical constituents and their inherent and apparent optical properties throughout the annual cycle of the North Atlantic plankton bloom using bio-optical data from four cruises conducted as part of the North Atlantic Aerosols and Marine Ecosystems Study (NAAMES). Our results show ocean color variability, quantified using field observations of the remote sensing reflectance spectrum at each NAAMES station, is driven by colored dissolved organic matter (CDOM) absorption in the ultraviolet wavelengths, phytoplankton absorption in the blue wavelengths, and total particulate backscattering in the green wavelengths. Results from a recently storm-mixed station at the height of the spring bloom demonstrate that significant changes in bio-optical properties can occur on daily scales. By testing the effects of variations in lighting conditions and solar geometries, we also demonstrate that, for this data set, remote sensing reflectance should be considered a quasi-inherent optical property.We find that the temporal and spatial chlorophyll concentrations and the magnitudes of inherent optical properties can be accurately assessed using previously published ocean color algorithms.However, changes in the spectral slopes of the inherent optical properties are often poorly retrieved, indicating the need for improvements in the retrieval of optical constituent composition.The characterization of such a dynamic environment provides beneficial insights for future biooptical algorithms.

Highlights

  • Algal blooms are driven by a complicated array of biological, chemical, and physical dynamics governing the growth and loss rates of phytoplankton (e.g., Sverdrup, 1953; Siegel et al, 2002; Behrenfeld and Boss, 2018)

  • Each of the four cruises captures a snapshot of the recurring annual bloom cycle, which to first order is reflected in the surface chlorophyll concentrations along latitudinal gradients (Table 1)

  • The range of biological states measured during North Atlantic Aerosols and Marine Ecosystems Study (NAAMES) makes it a very useful data set for the testing of satellite ocean color algorithms

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Summary

Introduction

Algal blooms are driven by a complicated array of biological, chemical, and physical dynamics governing the growth and loss rates of phytoplankton (e.g., Sverdrup, 1953; Siegel et al, 2002; Behrenfeld and Boss, 2018). The NAAMES project presents a unique opportunity to outline relationships between the optical properties of in-water constituents and ocean color over a diverse set of bloom states and lighting conditions It serves as a useful benchmark to test the retrievals of satellite products from empirical and semi-analytical bio-optical algorithms (IOCCG, 2006). Empirical algorithms, such as the OC Chlorophyll algorithm (O’Reilly et al, 1998; Werdell and Bailey, 2005), directly relate global matchups of bio-optical products and ocean color observations; while semi-analytical algorithms (e.g., Loisel and Stramski, 2000; Maritorena et al, 2002; Lee et al, 2014) use a combination of empirical relationships and theoretical expressions to determine the contributions of ocean constituents to ocean color spectra The performance of both types of algorithms can be limited by assumptions about the relationships between radiometric variables and their underlying optical constituents (Werdell et al, 2018). Validating and improving these bio-optical algorithms with in situ data will lead to enhanced characterization of regional to global scale models of phytoplankton dynamics (Siegel et al, 2013) and marine productivity (Behrenfeld et al, 2005; Westberry et al, 2008)

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