Abstract

Abstract. Multispectral information from satellite borne ocean colour sensors is at present used to characterize natural waters via the retrieval of concentrations of the three dominant optical constituents; pigments of phytoplankton, non-algal particles and coloured dissolved organic matter. A limitation of this approach is that accurate retrieval of these constituents requires detailed local knowledge of the specific absorption and scattering properties. In addition, the retrieval algorithms generally use only a limited part of the collected spectral information. In this paper we present an additional new algorithm that has the merit of using the full spectral information in the visible domain to characterize natural waters in a simple and globally valid way. This Forel–Ule MERIS (FUME) algorithm converts the normalized multiband reflectance information into a discrete set of numbers using uniform colourimetric functions. The Forel–Ule (FU) scale is a sea colour comparator scale that has been developed to cover all possible natural sea colours, ranging from indigo blue (the open ocean) to brownish-green (coastal water) and even brown (humic-acid dominated) waters. Data using this scale have been collected since the late nineteenth century, and therefore, this algorithm creates the possibility to compare historic ocean colour data with present-day satellite ocean colour observations. The FUME algorithm was tested by transforming a number of MERIS satellite images into Forel–Ule colour index images and comparing in situ observed FU numbers with FU numbers modelled from in situ radiometer measurements. Similar patterns and FU numbers were observed when comparing MERIS ocean colour distribution maps with ground truth Forel–Ule observations. The FU numbers modelled from in situ radiometer measurements showed a good correlation with observed FU numbers (R2 = 0.81 when full spectra are used and R2 = 0.71 when MERIS bands are used).

Highlights

  • The application of optical satellite remote sensing techniques to monitor the radiation scattered back from the water column became a major breakthrough in the seventies for monitoring ocean, sea and coastal areas (IOCCG, 1998)

  • In this paper an algorithm is presented that allows retrieval of the Forel–Ule sea colour from the MERIS satellite sensor

  • The elegance of our algorithm is that it converts multispectral observations to one simple number that is only dependent on a well-known universal set of colourimetric functions

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Summary

Introduction

The application of optical satellite remote sensing techniques to monitor the radiation scattered back from the water column became a major breakthrough in the seventies for monitoring ocean, sea and coastal areas (IOCCG, 1998). In 2002, of the MERIS instrument (Rast et al, 1999), which measures water-leaving reflectance in fifteen spectral bands with high signal-to-noise, it became possible to collect water-leaving radiance with high confidence in regional seas and coastal waters. This has led to the development of many new algorithms that can retrieve the phytoplankton pigments, and the mass concentration of suspended material and the absorption by dissolved material (Van der Woerd and Pasterkamp, 2008; Odermat et al, 2012).

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