Handout (2.2 MB)
Accurately correcting atmospheric effects in optically complex waters is a significant challenge, especially for high-precision applications like chl-a detection. Technical limitations such as spatial resolution, cloud coverage, and data accuracy hinder the broader use of satellite remote sensing. Furthermore, validating satellite-derived chl-a data requires accurate in situ measurements to minimize error propagation and ensure reliable assessments.
This study leverages recent remote sensing satellite series, including Landsat 8 and 9 data, as well as historical datasets from clear mesotrophic and oligotrophic lakes in the Adirondacks. The effectiveness of various atmospheric correction algorithms is evaluated by comparing satellite-derived chl-a estimates with in situ measurements. Preliminary results reveal significant variations in algorithm performance, particularly in their ability to detect chl-a accurately. While algorithms are sensitive to water color variations on an individual lake scale, stronger correlations between estimated and measured chl-a are observed in larger lakes. These findings emphasize the importance of selecting appropriate atmospheric correction techniques tailored to specific lake characteristics and conditions for accurate chl-a monitoring.
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