2021
DOI: 10.3390/atmos12121563
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Turbulence of Landward and Seaward Wind during Sea-Breeze Days within the Lower Atmospheric Boundary Layer

Abstract: 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 characterization of energy redistribution by turbulent eddies. The sea-breeze (SB) events were identified using a change in wind direction from seaward (SWD) to landward (LWD) during the day time. We found that the … Show more

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Cited by 3 publications
(4 citation statements)
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“…The cell state in one LSTM block is updated by four interacting layers, namely, forgetting gate, input gate, cell state updating, and output gate. Equations involved in these gates are detailed in [3]. Note that a number of trials with hidden units was made to optimize the hyperparameter.…”
Section: Detection Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…The cell state in one LSTM block is updated by four interacting layers, namely, forgetting gate, input gate, cell state updating, and output gate. Equations involved in these gates are detailed in [3]. Note that a number of trials with hidden units was made to optimize the hyperparameter.…”
Section: Detection Methodsmentioning
confidence: 99%
“…During these events, changes in wind speed, direction, and turbulence parameters occur at a time scales smaller than one hour. As a result, NLLJ and SB may have some impacts on the power production of wind turbines and air quality [1][2][3].…”
Section: Introductionmentioning
confidence: 99%
“…Complex dynamical turbulent processes associated to the stratified turbulence under shear are observed in atmosphere and in industry. This kind of turbulence problem presents an attractive physical field as it plays a key role to improve our understanding of behaviors of geophysical flows [1][2][3][4]. Dynamical turbulent processes associated to the stratified turbulence submitted to an inclined shear are encountered in industry and atmosphere.…”
Section: Introductionmentioning
confidence: 99%
“…During SB the wind speed increases and the wind blows from the sea towards the land. This phenomenon occurs due to an adverse atmospheric pressure gradient generated by the temperature difference between land and sea (Augustin et al 2020, Mazon et al 2015, Roy et al 2021b during the daytime. During clear weather, after sunset, a strong wind acceleration can be observed around 50-1000 m above ground level (a.g.l.…”
Section: Introductionmentioning
confidence: 99%