Determination of reflectance of coral reefs through analysis of the diffuse attenuation coefficients for radiance through the water column

E. LeDrew, H. Holden
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引用次数: 1

Abstract

Summary form only given. Landsat Thematic Mapper and SPOT satellite image data have been used in a qualitative manner to map the spatial characteristics of tropical reef systems. Recently, data available for shallow corals have been studied to determine a "Living Madrepora Index" that may form the basis for quantitative analysis of ecosystem viability. This may be of particular importance in studies of coral bleaching events that may be caused by climate variability or change, and/or pollutant stress. The challenge is to adjust the digital imagery for the optical attenuation through water to greater depths with corrections that will vary with the density of intervening sediment or plankton. In this paper the authors report on a study in Fiji in which they measured the vertical profiles of the diffuse attenuation coefficient for upwelling radiance in the SeaWiFS channels. They discuss the properties of these coefficients and derivation of an image independent procedure for retrieval of the bottom upwelling radiance without correction for depth.
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通过分析通过水柱的辐射的扩散衰减系数来测定珊瑚礁的反射率
只提供摘要形式。Landsat专题制图器和SPOT卫星图像数据已被定性地用于绘制热带珊瑚礁系统的空间特征。最近,研究人员研究了浅层珊瑚的现有数据,以确定“活珊瑚指数”,这可能成为定量分析生态系统可行性的基础。这在研究可能由气候变率或变化和/或污染物胁迫引起的珊瑚白化事件时可能特别重要。面临的挑战是调整数字图像,使光学衰减通过水到更大的深度,校正将随着沉积物或浮游生物的密度而变化。在这篇论文中,作者报告了在斐济进行的一项研究,他们测量了SeaWiFS通道中上升流辐射的扩散衰减系数的垂直剖面。他们讨论了这些系数的性质,并推导了一个与图像无关的程序,用于检索底部上升流辐射,而不需要对深度进行校正。
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