Abstract

The aim of this research is to use hyperspectral MIVIS data to map the Posidonia oceanica prairies in a coastal lagoon (Stagnone di Marsala). It is approximately 12 km long and 2 km wide and is linked to the open sea by two shallow openings. This environment is characterised by prairies of phanerogams, the most common of which is Posidonia oceanica, an ideal habitat for numerous species of fish, molluscs and crustaceans. A knowledge of the distribution of submerged vegetation is useful to monitor the health of the lagoon. In order to classify the MIVIS imagery, the attenuation effects of the water column have been removed from the signal using Lyzenga’s technique. A comparison between classifications using indices obtained using band pairs from only the first spectrometer, and using band pairs of the first and second spectrometers, shows that the best classification is obtained from some indices derived from the first spectrometer. Field controls carried out in July 2002 were used to determine the training sites for the supervised classification. Twelve classes of bottom coverage were obtained from the classification, of which four are homogeneous and eight are mixed coverage. The methodology applied demonstrates that hyperspectral sensors can be used to effectively map submerged vegetation in shallow waters.

Highlights

  • Mapping the density and distribution of benthic vegetation is valuable for the monitoring and management of coastal areas as discussed later

  • The Lyzenga method is proposed as an alternative to water column correction using the Ben Moussa et al (1989) equation

  • The latter requires a knowledge of the bathymetry and attenuation coefficients with varying wavelengths, even a slight error in the bathymetry causes substantial over-correction of the influence of the water column since bathymetry is in the exponential term of the radiative transfer eq (3.1)

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Summary

Introduction

Mapping the density and distribution of benthic vegetation is valuable for the monitoring and management of coastal areas as discussed later. 1993; Ferguson and Korfmacher, 1997; Mumby et al, 1998; Durand et al, 2000; Holden and LeDrew, 2002; Dierssen et al, 2003; Louchard et al, 2003) using either satellite or aerial remote sensing data to study the distribution of benthic vegetation, coral or bed type in coastal areas Many of these studies have not attempted to take the attenuation effects of the overlying water column into account, others have used a variety of approaches to reduce the effects of the water column. The main disadvantage stated in using the Lyzenga (1981) method is that it is only reliable in clear waters and that most coastal waters are turbid (Durand et al, 2000)

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