Wave-Breaking Turbulence in the Ocean Surface Layer

Details

• Journal Title:
  Journal of Physical Oceanography
• Personal Author:
  Thomson, Jim ; Schwendeman, Michael S. ; Zippel, Seth F. ; Moghimi, Saeed ; Gemmrich, Johannes ; Rogers, W. Erick
• NOAA Program & Office:
  NOS (National Ocean Service) ; OCS (Office of Coast Survey)
• Description:
  Observations of winds, waves, and turbulence at the ocean surface are compared with several analytic formulations and a numerical model for the input of turbulent kinetic energy by wave breaking and the subsequent dissipation. The observations are generally consistent with all of the formulations, although some differences are notable at winds greater than 15 m s−1. The depth dependence of the turbulent dissipation rate beneath the waves is fit to a decay scale, which is sensitive to the choice of vertical reference frame. In the surface-following reference frame, the strongest turbulence is isolated within a shallow region of depths much less than one significant wave height. In a fixed reference frame, the strong turbulence penetrates to depths that are at least half of the significant wave height. This occurs because the turbulence of individual breakers persists longer than the dominant period of the waves and thus the strong surface turbulence is carried from crest to trough with the wave orbital motion.
• Source:
  Journal of Physical Oceanography, 46(6), 1857-1870
• DOI:
  https://doi.org/10.1175/JPO-D-15-0130.1
• ISSN:
  0022-3670 ; 1520-0485
• Format:
  pdf
• Publisher:
  American Meteorological Society
• Document Type:
  Journal Article
• Rights Information:
  Other
• Compliance:
  Submitted
• Main Document Checksum:
  urn:sha-512:19f1ea721ace38b5c38e85895de83e1a4194a2f49fe83a46f2bbf9ae9f0afa16b025b7b6776582bc8f26eaa7418bd57530de736693facf6858e1339eb94c7a6a
• Download URL:
  https://repository.library.noaa.gov/view/noaa/71308/noaa_71308_DS1.pdf
• File Type:
  [PDF - 1.34 MB ]