Lake Tahoe is known around the world for its famed water clarity, eliciting awe from millions of visitors each year. UC Davis researchers have been monitoring the changes in lake clarity for the past 50 years using a Secchi disk (the white dinner plate). From the late 1960's through the turn of the century, there was a decline in clarity brought about by increased algae growth and the presence of very fine particles. Over the past decade we have seen the rate of clarity decline ease with winter clarity actually improving. Using technology beyond the dinner plate, researchers continue to refine their understanding of lake physics and ecology to determine the cause of annual clarity change, enabling management agencies to focus on the most pressing issues effecting Tahoe's clarity.
In 2014 the annual average Secchi depth was 77.8 feet (23.7 meters), an increase of approximately 7 feet over the previous year. It is important to understand the causes behind clarity change and to evaluate past actions and future investments.