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Seabed stress determinations using the inertial dissipation method and the turbulent kinetic energy method
Author(s) -
Stapleton K. R.,
Huntley D. A.
Publication year - 1995
Publication title -
earth surface processes and landforms
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.294
H-Index - 127
eISSN - 1096-9837
pISSN - 0197-9337
DOI - 10.1002/esp.3290200906
Subject(s) - dissipation , seabed , turbulence kinetic energy , kinetic energy , turbulence , current meter , inertial frame of reference , stress (linguistics) , energy (signal processing) , field (mathematics) , geology , mechanics , marine engineering , acoustics , environmental science , physics , classical mechanics , engineering , mathematics , oceanography , linguistics , philosophy , quantum mechanics , pure mathematics , thermodynamics
Direct measurements of seabed stress are difficult, especially in field conditions. Several methods for estimating these stresses using current meter data are available. Two of these methods, the Inertial Dissipation Method and the Turbulent Kinetic Energy Method, are described below, and a Matlab program is used to analyse data from a wave‐current environment.

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