Abstract

Abstract: The chlorophyll-a (Chla) products of seven processors developed for the Medium Resolution Imaging Spectrometer (MERIS) sensor were evaluated. The seven processors, based on a neural network and band height, were assessed over an optically complex water body with Chla concentrations of 8.10–187.40 mg∙m−3 using 10-year MERIS archival data. These processors were adopted for the Ocean and Land Color Instrument (OLCI) sensor. Results indicated that the four processors of band height (i.e. the Maximum Chlorophyll Index (MCI_L1); and Fluorescence Line Height (FLH_L1)); neural network (i.e. Eutrophic Lake (EUL); and Case 2 Regional (C2R)) possessed reasonable retrieval accuracy with root mean square error (R2) in the range of 0.42–0.65. However, these processors underestimated the retrieved Chla > 100 mg∙m−3, reflecting the limitation of the band height processors to eliminate the influence of non-phytoplankton matter and highlighting the need to train the neural network for highly turbid waters. MCI_L1 outperformed other processors during the calibration and validation stages (R2 = 0.65, Root mean square error (RMSE) = 22.18 mg∙m−3, the mean absolute relative error (MARE) = 36.88%). In contrast, the results from the Boreal Lake (BOL) and Free University of Berlin (FUB) processors demonstrated their inadequacy to accurately retrieve Chla concentration > 50 mg∙m−3, mainly due to the limitation of the training datasets that resulted in a high MARE for BOL (56.20%) and FUB (57.00%). Mapping the spatial distribution of Chla concentrations across Lake Kasumigaura using the seven processors showed that all processors—except for the BOL and FUB—were able to accurately capture the Chla distribution for moderate and high Chla concentrations. In addition, MCI_L1 and C2R processors were evaluated over 10-years of monthly measured Chla as they demonstrated the best retrieval accuracy from both groups (i.e. band height and neural network, respectively). The retrieved Chla of MCI_L1 was more accurate at tracking seasonal and annual variation in Chla than C2R, with only slight overestimation occurring during the springtime.

Highlights

  • The concentration of water constituents can fluctuate significantly over a short time period, making it necessary to continuously monitor bodies of water [1]

  • An evaluation of five out of the seven processors that provide direct Chla concentrations revealed that these processors tended to underestimate (EUL, Boreal Lake (BOL), Case 2 Regional (C2R), and Free University of Berlin (FUB)), or overestimate (MPH) the retrieved Chla

  • The Eutrophic Lake (EUL), C2R, MCI_L1, and FLH_L1 provided acceptable accuracies for the validation stage, they underestimated the retrieved Chla for Chla concentrations > 100 mg·m−3. These results revealed the limitations of band height algorithms to eliminate the influence of other constituents, with high concentrations as reported by [13] and emphasize the importance of including high Chla concentration during the training stage of neural networks (NN) processors, especially before incorporating these processors with the Ocean and Land Color Instrument (OLCI) sensor

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Summary

Introduction

The concentration of water constituents can fluctuate significantly over a short time period, making it necessary to continuously monitor bodies of water [1]. Chla retrieval in turbid waters shifts from the blue and green to the red and NIR spectral region to avoid high absorption of colored dissolved organic matter (CDOM) and non-algal particles (NAP) [8,9,10]. Monitoring the water quality of oceans from space started in 1978 with the use of the Coastal Zone Color Scanner (CZCS) sensor [11,12,13,14]. Several other ocean color sensors such as the Sea-viewing Wide Field-of-view (SeaWiFS), Moderate Resolution Imaging Spectroradiometer (MODIS), and Medium Resolution Imaging Spectrometer (MERIS) have been employed to monitor water quality of the open ocean as well as inland lakes [15,16]. The floating brown algae Sargassum was first detected from space using the 709-nm band [20]

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