“…As light travels through the water column it interacts with both molecules and particles that comprise the chlorophyll (chl), colored dissolved organic matter (cdom) and inorganic suspended minerals (sm) resulting in alterations of the upwelling radiative flux (Pozdnyakov and Grassel, 2003). Thus the backscattered flux emerging from beneath the water surface contains information about the optical properties of the water column which when observed over time provides insight into the dynamic processes of the Great Lakes (Shuchman et al, 2006).…”