Abstract

Remote sensing is playing an increasingly important role in the monitoring and management of coastal regions, coral reefs, inland lakes, waterways, and other shallow aquatic environments. Ongoing advances in algorithm development, sensor technology, computing capabilities, and data availability are continuing to improve our ability to accurately derive information on water properties, water depth, benthic habitat composition, and ecosystem health. However, given the physical complexity and inherent variability of the aquatic environment, most of the remote sensing models used to address these challenges require localized input parameters to be effective and are thereby limited in geographic scope. Additionally, since the parameters in these models are interconnected, particularly with respect to bathymetry, errors in deriving one parameter can significantly impact the accuracy of other derived parameters and products. This study utilizes hyperspectral data acquired in Hawaii in 2000–2001 and 2017–2018 using NASA’s Classic Airborne Visible/Infrared Imaging Spectrometer to evaluate performance and sensitivity of a well-established semi-analytical inversion model used in the assessment of coral reefs. Analysis is performed at several modeled spatial resolutions to emulate characteristics of different feasible moderate resolution hyperspectral satellites, and data processing is approached with the objective of developing a generalized, scalable, automated workflow. Accuracy of derived water depth is evaluated using bathymetric lidar data, which serves to both validate model performance and underscore the importance of image quality on achieving optimal model output. Data are then used to perform a sensitivity analysis and develop confidence levels for model validity and accuracy. Analysis indicates that derived benthic reflectance is most sensitive to errors in bathymetry at shallower depths, yet remains significant at all depths. The confidence levels provide a first-order method for internal quality assessment to determine the physical extent of where and to what degree model output is considered valid. Consistent results were found across different study sites and different spatial resolutions, confirming the suitability of the model for deriving water depth in complex coral reef environments, and expanding our ability to achieve automated widespread mapping and monitoring of global coral reefs.

Highlights

  • This study utilizes hyperspectral data acquired in Hawaii in 2000–2001 and 2017–2018 using National Aeronautics and Space Administration (NASA)’s Classic Airborne Visible/Infrared Imaging Spectrometer to evaluate performance and sensitivity of a well-established semi-analytical inversion model used in the assessment of coral reefs

  • Deriving bathymetry from remote sensing data has long played an important role in the study of coastal regions, coral reefs, inland lakes, waterways, and other aquatic areas

  • The accuracy of remote sensing-derived bathymetry using multispectral and hyperspectral passive optical sensors is affected by several factors, especially variations in water properties and benthic composition

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Summary

Introduction

Deriving bathymetry from remote sensing data has long played an important role in the study of coastal regions, coral reefs, inland lakes, waterways, and other aquatic areas. Multispectral and hyperspectral remote sensing-derived bathymetry is not commonly used in navigation charting (e.g., shipping channels) [3], where high accuracy is required, and performs best in areas with uniform substrate at less than 20 m depth. Because of these limitations, it is more difficult to accurately derive bathymetry using passive optical remote sensing techniques in areas with heterogeneous bottom surfaces such as coral reefs [17]

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