Researchers with the Environmental Physics Group at the University of Konstanz investigated the properties of solitary-like waves in Lake Constance over several years using a T-Chain.
They are particularly interested in the occurrence of large internal waves because these affect mixing in the thermocline via breaking.
In order to generate data, they deployed a PME T-Chain for over six years in the center of a sub basin Lake Constance, Germany. The T-Chain measured temperature every minute. The accuracy of at least 0.02 °C over the six years allowed the identification of large-scale temperature overturns in association with solitary-like waves.
The contour plots to the right demonstrate the strengthening of stratification during Spring together with several cycles of basin-scale internal seiche and the passage of a solitary-like wave train. |