Turbulent benthic boundary layer mixing events in fresh water lakes

C Lemckert, J Imberger

    Research output: A Conference proceeding or a Chapter in BookChapter

    Abstract

    The nature of the turbulent benthic boundary later (TBBL) within thermally stratified lakes was investigated using data collected from two field studies. A profiling instrument was used to record the turbulent properties of the layers, while thermistor chains were used to monitor the internal wave field. The results obtained indicated that in these studies the TBBLs were generated by internal waves as they progressed over the sloping beds of the lakes. The mixing efficiency of the turbulent events associated with the TBBL was found to be dependent on the turbulent Froude number. The findings indicate that the TBBL's were very important vertical turbulent transport mechanism
    Original languageEnglish
    Title of host publicationPhysical Processes in Lakes and Oceans
    EditorsJorg Imberger, Malclom J. Brown, Christopher N. K. Mooers
    Place of PublicationUnited States of America
    PublisherAmerican Geophysical Union
    Chapter35
    Pages503-516
    Volume54
    ISBN (Electronic)9781118665381
    ISBN (Print)9780875902685
    DOIs
    Publication statusPublished - 1998

    Publication series

    NameCOASTAL AND ESTUARINE STUDIES

    Cite this

    Lemckert, C., & Imberger, J. (1998). Turbulent benthic boundary layer mixing events in fresh water lakes. In J. Imberger, M. J. Brown, & C. N. K. Mooers (Eds.), Physical Processes in Lakes and Oceans (Vol. 54, pp. 503-516). (COASTAL AND ESTUARINE STUDIES). American Geophysical Union. https://doi.org/10.1029/CE054p0503