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Scientific Investigations Report 2010–5203


Use of Acoustic Backscatter and Vertical Velocity to Estimate Concentration and Dynamics of Suspended Solids in Upper Klamath Lake, South-Central Oregon: Implications for Aphanizomenon flos-aquae

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Figure 2. Diel patterns in the difference between water temperatures measured near-surface and near-bottom at sites MDN (4.5 m depth), EPT (12.5 m depth), and MDT (14.8 m depth) in Upper Klamath Lake, south-central Oregon. Diel patterns are derived from an average of hourly monitor measurements between June 2, 2005, and October 9, 2005. Minimum temperature differences occur between 07:00 h (sites MDN and EPT) and 08:00 h (site MDT); maximum temperature differences occur between 16:00 h (site MDN) and 19:00 h (site MDT). The maximum standard error of the estimate of the average temperature difference is 0.07 ºC at sites EPT and MDN, and 0.14 °C at site MDT.


First posted March 16, 2011

For additional information contact:
Director, Oregon Water Science Center
U.S. Geological Survey
2130 SW 5th Avenue
Portland, Oregon 97201
http://or.water.usgs.gov

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