A method to determine the characteristic time‐scales of quasi‐isotropic surface‐layer turbulence over complex terrain: A case‐study in the Adige Valley (Italian Alps)

Author:

Falocchi Marco12ORCID,Giovannini Lorenzo1ORCID,de Franceschi Massimiliano3ORCID,Zardi Dino12ORCID

Affiliation:

1. Atmospheric Physics Group, Department of Civil, Environmental and Mechanical Engineering, University of Trento, Trento, Italy

2. C3A – Center Agriculture Food Environment, University of Trento, Trento, Italy

3. Diocese of Bolzano–Bressanone, Bolzano, Italy

Publisher

Wiley

Subject

Atmospheric Science

Reference74 articles.

1. Anisotropy stress invariants of thermally stratified wind turbine array boundary layers using large‐eddy simulations;Ali N.;Journal of Renewable and Sustainable Energy,2018

2. American Meteorological Society(2012).Glossary of Meteorology.

3. An Analysis Of Sonic Anemometer Observations In Low Wind Speed Conditions

4. Turbulence kinetic energy budget in the stable boundary layer over a heterogeneous surface

5. Determining a turbulence averaging time‐scale by Fourier analysis for the nocturnal boundary layer;Babić K.;Geofizika,2012

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