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Vertical Structure in the Marine Atmospheric Boundary Layer and its Implication for the Inertial Dissipation Method

✍ Scribed by Anna Sjöblom; Ann-Sofi Smedman

Book ID
111550350
Publisher
Springer
Year
2003
Tongue
English
Weight
238 KB
Volume
109
Category
Article
ISSN
0006-8314

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The dissipation rate of turbulent kinetic energy, E, and the temperature structure function parameter, C& have been measured over water from the near surface (Z = 3 m) to the top of the boundary layer. The near surface values of E and C; were used to calculate the velocity and temperature Monin Obuk