Articles | Volume 9, issue 2
https://doi.org/10.5194/essd-9-497-2017
https://doi.org/10.5194/essd-9-497-2017
25 Jul 2017
 | 25 Jul 2017

Expanding understanding of optical variability in Lake Superior with a 4-year dataset

Colleen B. Mouw, Audrey B. Ciochetto, Brice Grunert, and Angela Yu

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Cited articles

APHA/AWWA/WEF – American Public Health Association, American Water Works Association and Water Environment Federation: Standard Methods for the Examination of Water and Wastewater, in: 21st Edn., Sections 2540A Solids, 2540C Total Suspended Solids Dried at 103–105 °C and 2540E Fixed and Volatile Solids Ignited at 550 °C, Washington, D.C., 2005.
Assel, R. A.: Fall and winter thermal structure of Lake Superior, J. Great Lakes Res., 12, 251–262, https://doi.org/10.1016/S0380-1330(86)71725-5, 1986.
Austin, J. A. and Allen, J.: Sensitivity of summer Lake Superior thermal structure to meteorological forcing, Limnol. Oceanogr., 56, 1141–1154, 2011.
Austin, J. A. and Colman, S. M.: Lake Superior summer water temperatures are increasing more rapidly than regional air temperatures: A positive ice-albedo feedback, Geophys. Res. Lett., 34, L06604, https://doi.org/10.1029/2006GL029021, 2007.
Barbiero, R. P. and Tuchman, M. L.: Results from the U.S. EPA's biological open water surveillance program of the Laurentian great lakes: I. Introduction and Phytoplankton Results, J. Great Lakes Res., 27, 134–154, 2001.
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Short summary
Lake Superior is one of the largest freshwater lakes on our planet, but few optical observations have been made to allow for the development and validation of visible spectral satellite remote sensing products. The dataset described here focuses on coincidently observing optical properties along with biogeochemical parameters and substantially increases the optical knowledge of the lake.
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