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Estimation of turbulence kinetic energy dissipation rate in a Bora event (CROSBI ID 528603)

Prilog sa skupa u zborniku | izvorni znanstveni rad | međunarodna recenzija

Večenaj, Željko ; Belušić, Danijel ; Grisogono, Branko Estimation of turbulence kinetic energy dissipation rate in a Bora event // 29th International Conference on Alpine Meteorology - Extended Abstracts. Météo-France, 2007. str. 745-748-x

Podaci o odgovornosti

Večenaj, Željko ; Belušić, Danijel ; Grisogono, Branko

engleski

Estimation of turbulence kinetic energy dissipation rate in a Bora event

During a bora event, the turbulence is strongly developed in the lee of the mountain. Wind speed at Senj was measured at 13 m above the ground with a 3D ultrasonic anemometer operating at 4 Hz sampling frequency. This data was used for evaluation of the turbulent kinetic energy (TKE) dissipation rate ε . The estimated value of ε with the inertial dissipation method (IDM) for this event is 1.22 m^2 s^-3 and is taken as the reliable one. An alternative method is based on the third-order streamwise velocity structure function (3SF) which requires a local turbulence isotropy. Using this approach a significantly lower value of ε is obtained, not surpassing 0.70 m^2 s^-3. Inspecting the stronger isotropy condition for the inertial subrange, i.e. the 4:3 ratio of vertical and transverse to streamwise velocity spectra, it is found that the present anemometer's sampling rate only approaches the inertial subrange. This partly explains the lower value of ε obtained using the second method. Thus, the anemometer of a much higher sampling frequency is needed for further studies of the bora-related small-scale turbulence.

bora wind; dissipation rate; inertial dissipation technique; structure function; local isotropy

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Podaci o prilogu

745-748-x.

2007.

objavljeno

Podaci o matičnoj publikaciji

29th International Conference on Alpine Meteorology - Extended Abstracts

Météo-France

Podaci o skupu

29th International Conference on Alpine Meteorology

poster

04.06.2007-08.06.2007

Chambéry, Francuska

Povezanost rada

Geologija

Poveznice