Abstract

Human activity and natural climate trends constitute a major threat to coral reefs worldwide. Models predict a significant reduction in reef spatial extension together with a decline in biodiversity in the relatively near future. In this context, monitoring programs to detect changes in reef ecosystems are essential. In recent years, coral reef mapping using remote sensing data has benefited from instruments with better resolution and computational advances in storage and processing capabilities. However, the water column represents an additional complexity when extracting information from submerged substrates by remote sensing that demands a correction of its effect. In this article, the basic concepts of bottom substrate remote sensing and water column interference are presented. A compendium of methodologies developed to reduce water column effects in coral ecosystems studied by remote sensing that include their salient features, advantages and drawbacks is provided. Finally, algorithms to retrieve the bottom reflectance are applied to simulated data and actual remote sensing imagery and their performance is compared. The available methods are not able to completely eliminate the water column effect, but they can minimize its influence. Choosing the best method depends on the marine environment, available input data and desired outcome or scientific application.

Highlights

  • Coral reefs are the most biodiverse and productive ecosystems in marine environments [1]

  • Several studies have shown that these ecosystems appear to be the first to respond to global climate changes, such as increased sea surface temperature (SST) and ultraviolet radiation (UV) and acidification of seawater that results from higher levels of atmospheric CO2 concentration

  • Among all the methods developed to date, none are generally capable of correcting for the water column effect properly in the entire visible spectrum

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Summary

Introduction

Coral reefs are the most biodiverse and productive ecosystems in marine environments [1]. Several studies have shown that these ecosystems appear to be the first to respond to global climate changes, such as increased sea surface temperature (SST) and ultraviolet radiation (UV) and acidification of seawater that results from higher levels of atmospheric CO2 concentration. SST increases can lead to a loss of symbiotic relationships between corals and zooxanthells and cause coral bleaching events. Coral reefs are considered to act as biological indicators of global climate change [3]. In this context, monitoring programs to detect changes in coral reef biodiversity and coral bleaching are essential

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