TY - JOUR
T1 - Estimation of Diffuse Attenuation of Ultraviolet Light in Optically Shallow Florida Keys Waters from Modis Measurements
AU - Barnes, Brian Burnel
AU - Hu, Chuanmin
AU - Cannizzaro, Jennifer P.
AU - Craig, Susanne E.
AU - Jones, David L.
AU - Lehrter, John C.
AU - Melo, Nelson
AU - Schaeffer, Blake A.
AU - Zepp, Richard
PY - 2014/1/1
Y1 - 2014/1/1
N2 - Diffuse attenuation of solar light ( K d , m −1 ) determines the percentage of light penetrating the water column and available for benthic organisms. Therefore, K d can be used as an index of water quality for coastal ecosystems that are dependent on photosynthesis , such as the coral reef environments of the Florida Reef Tract. Ultraviolet (UV) light reaching corals can lead to reductions in photosynthetic capacity as well as DNA damage. Unfortunately, field measurements of K d (UV) lack sufficient spatial and temporal coverage to derive statistically meaningful patterns, and it has been notoriously difficult to derive K d in optically shallow waters from remote sensing due to bottom contamination . Here we describe an approach to derive K d (UV) in optically shallow waters of the Florida Keys using variations in the spectral shape of MODIS-derived surface reflectance . The approach used a principal component analysis and stepwise multiple regression to parsimoniously select modes of variance in MODIS-derived reflectance data that best explained variance in concurrent in situ K d (UV) measurements. The resulting models for K d (UV) retrievals in waters 1–30 m deep showed strong positive relationships between derived and measured parameters [ e.g. , for K d (305) ranging from 0.28 to 3.27 m −1 ; N = 29; R 2 = 0.94]. The predictive capabilities of these models were further tested, also showing acceptable performance [for K d (305), R 2 = 0.92; bias = − 0.02 m −1 ; URMS = 23%]. The same approach worked reasonably well in deriving the absorption coefficient of colored dissolved organic matter (CDOM) in UV wavelengths [ a g(UV), m −1 ], as K d (UV) is dominated by a g (UV). Application of the approach to MODIS data showed different spatial and temporal K d (305) patterns than the K d (488) patterns derived from a recently validated semi-analytical approach, suggesting that different mechanisms are controlling K d in the UV and in the visible. Given the importance of water clarity and light availability to shallow-water flora and fauna, the new K d (UV) and a g (UV) data products provide unprecedented information for assessing and monitoring of coral reef health, and could further assist ongoing regional protection efforts.
AB - Diffuse attenuation of solar light ( K d , m −1 ) determines the percentage of light penetrating the water column and available for benthic organisms. Therefore, K d can be used as an index of water quality for coastal ecosystems that are dependent on photosynthesis , such as the coral reef environments of the Florida Reef Tract. Ultraviolet (UV) light reaching corals can lead to reductions in photosynthetic capacity as well as DNA damage. Unfortunately, field measurements of K d (UV) lack sufficient spatial and temporal coverage to derive statistically meaningful patterns, and it has been notoriously difficult to derive K d in optically shallow waters from remote sensing due to bottom contamination . Here we describe an approach to derive K d (UV) in optically shallow waters of the Florida Keys using variations in the spectral shape of MODIS-derived surface reflectance . The approach used a principal component analysis and stepwise multiple regression to parsimoniously select modes of variance in MODIS-derived reflectance data that best explained variance in concurrent in situ K d (UV) measurements. The resulting models for K d (UV) retrievals in waters 1–30 m deep showed strong positive relationships between derived and measured parameters [ e.g. , for K d (305) ranging from 0.28 to 3.27 m −1 ; N = 29; R 2 = 0.94]. The predictive capabilities of these models were further tested, also showing acceptable performance [for K d (305), R 2 = 0.92; bias = − 0.02 m −1 ; URMS = 23%]. The same approach worked reasonably well in deriving the absorption coefficient of colored dissolved organic matter (CDOM) in UV wavelengths [ a g(UV), m −1 ], as K d (UV) is dominated by a g (UV). Application of the approach to MODIS data showed different spatial and temporal K d (305) patterns than the K d (488) patterns derived from a recently validated semi-analytical approach, suggesting that different mechanisms are controlling K d in the UV and in the visible. Given the importance of water clarity and light availability to shallow-water flora and fauna, the new K d (UV) and a g (UV) data products provide unprecedented information for assessing and monitoring of coral reef health, and could further assist ongoing regional protection efforts.
KW - coral reef
KW - light penetration
KW - remote sensing
KW - shallow water
KW - ultra-violet light
KW - water clarity
UR - https://digitalcommons.usf.edu/msc_facpub/917
UR - https://doi.org/10.1016/j.rse.2013.09.024
U2 - 10.1016/j.rse.2013.09.024
DO - 10.1016/j.rse.2013.09.024
M3 - Article
VL - 140
JO - Remote Sensing of Environment
JF - Remote Sensing of Environment
ER -