2011
DOI: 10.1016/j.enconman.2010.10.014
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Vertical characterization of the wind mode and its effect on the wind farm profitability of Sidi Daoud – Tunisia

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Cited by 19 publications
(13 citation statements)
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“…The standard height of measurement is generally of 10 m, but during a prospection of a site, in order to draw up a wind project, it is preferable to take measures at two or three levels for one period at least six months in order to know the evolution of the wind speed at altitudes representing an energy interest. The majority of work on the determination of the wind vertical profile in the surface boundary layer is based on the similarity theory of Monin-Obukov [22][23]. This theory was supplemented by studies which proposed extrapolation laws of the wind speed of a level H 1 on a level H 1 according to the variation of roughness classes.…”
Section: Vertical Extrapolation Of the Wind Speed 41 Extrapolation Lawsmentioning
confidence: 99%
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“…The standard height of measurement is generally of 10 m, but during a prospection of a site, in order to draw up a wind project, it is preferable to take measures at two or three levels for one period at least six months in order to know the evolution of the wind speed at altitudes representing an energy interest. The majority of work on the determination of the wind vertical profile in the surface boundary layer is based on the similarity theory of Monin-Obukov [22][23]. This theory was supplemented by studies which proposed extrapolation laws of the wind speed of a level H 1 on a level H 1 according to the variation of roughness classes.…”
Section: Vertical Extrapolation Of the Wind Speed 41 Extrapolation Lawsmentioning
confidence: 99%
“…The modeling of the vertical profile of the wind speed in the measurement place mast 4 by the power and logarithmic laws, in order to know the evolution the wind speed at altitudes representing an energy interest [22][23][24][25][26][27]. A close attention is paid to the study of the influence height on the wind characteristics (mean speed and power density) by using the Rayleigh distribution.…”
Section: Fig 1 Energy Resources and Demand In Tunisiamentioning
confidence: 99%
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“…It is located between altitude 30˚N and 37˚N latitude and between 8˚E and 12˚E longitude [4,[9][10][11]. Its littoral extends on 1300 km and comprises five large gulfs.…”
Section: Geographical Situation and Relief Of Tunisiamentioning
confidence: 99%
“…The Von Karman theory showed that, for a flow under constant flux and neutral atmospheric conditions, the profile of the wind speed is a logarithmic curve of the form [11][12][13][14][15]:…”
Section: Influence Of Height On the Wind Resourcementioning
confidence: 99%