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Turbulence of Landward and Seaward Wind during Sea-Breeze Days within the Lower Atmospheric Boundary Layer

Reynolds stress anisotropy is estimated from the stress spheroids, based on 20 Hz ultrasonic anemometer measurements, performed in the coastal area of northern France, over a 1.5-year long period. Size and shape variation (i.e., prolate, oblate, disk, rod, etc.) of stress spheroids are used for the...

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Principais autores: Sayahnya Roy, Alexei Sentchev, Marc Fourmentin, Patrick Augustin
Format: Artigo
Sprog:Inglês
Udgivet: MDPI AG 2021-11-01
Serier:Atmosphere
Fag:
kinetic energy flux
reynolds stress anisotropy
sea-breeze circulation
turbulence
ultrasonic anemometer
Online adgang:https://www.mdpi.com/2073-4433/12/12/1563
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