Articles | Volume 21, issue 1
https://doi.org/10.5194/hess-21-377-2017
https://doi.org/10.5194/hess-21-377-2017
Research article
 | 
24 Jan 2017
Research article |  | 24 Jan 2017

Satellite-derived light extinction coefficient and its impact on thermal structure simulations in a 1-D lake model

Kiana Zolfaghari, Claude R. Duguay, and Homa Kheyrollah Pour

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Cited articles

Armengol, J., Caputo, L., Comerma, M., Feijoó, C., García, J. C., Marcé, R., Navarro, E., and Ordoñez, J.: Sau reservoir's light climate: relationships between Secchi depth and light extinction coefficient, Limnetica, 22, 195–210, 2003.
Arst, H., Erm, A., Herlevi, A., Kutser, T., Leppäranta, M., Reinart, A., and Virta, J.: Optical properties of boreal lake waters in Finland and Estonia, Boreal Environ. Res., 13, 133–158, 2008.
Attila, J., Koponen, S., Kallio, K., Lindfors, A., Kaitala, S., and Ylostalo, P.: MERIS Case II water processor comparison on coastal sites of the northern Baltic Sea, Remote Sens. Environ., 128, 138–149, 2013.
Binding, C. E. Jerome, J. H., Bukata, R. P., and Booty, W. G.: Trends in water clarity of the lower Great Lakes from remotely sensed aquatic color, J. Great Lakes Res., 33, 828–841, 2007.
Binding, C. E., Greenberg, T. A., Watson, S. B., Rastin, S., and Gould, J.: Long term water clarity changes in North America's Great Lakes from multi-sensor satellite observations, Limnol. Oceanogr., 60, 1967–1995, 2015.
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Short summary
A remotely-sensed water clarity value (Kd) was applied to improve FLake model simulations of Lake Erie thermal structure using a time-invariant (constant) annual value as well as monthly values of Kd. The sensitivity of FLake model to Kd values was studied. It was shown that the model is very sensitive to variations in Kd when the value is less than 0.5 m-1.