Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)

This paper deals with the characteristics of turbulent flow over two agricultural plots with various tillage treatments in a fallow, semiarid area (Central Aragon, Spain). The main dynamic characteristics of the Atmospheric Surface Layer (ASL) measured over the experimental site (friction ve...

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Main Authors: S. Yahaya, J. P. Frangi, D. C. Richard
Format: Article
Language:English
Published: Copernicus Publications 2003-10-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/21/2119/2003/angeo-21-2119-2003.pdf
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spelling doaj-350e09d431a84e0e9d4f43313ef5ca352020-11-24T23:46:42ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762003-10-01212119213110.5194/angeo-21-2119-2003Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)S. Yahaya0J. P. Frangi1D. C. Richard2Laboratoire Environnement and Développement, CP 7071 Université Denis Diderot (Paris 7), 2 Place Jussieu, 75251 Paris Cedex 05, FranceLaboratoire Environnement and Développement, CP 7071 Université Denis Diderot (Paris 7), 2 Place Jussieu, 75251 Paris Cedex 05, FranceLaboratoire Environnement and Développement, CP 7071 Université Denis Diderot (Paris 7), 2 Place Jussieu, 75251 Paris Cedex 05, FranceThis paper deals with the characteristics of turbulent flow over two agricultural plots with various tillage treatments in a fallow, semiarid area (Central Aragon, Spain). The main dynamic characteristics of the Atmospheric Surface Layer (ASL) measured over the experimental site (friction velocity, roughness length, etc.), and energy budget, have been presented previously (Frangi and Richard, 2000). The current study is based on experimental measurements performed with cup anemometers located in the vicinity of the ground at 5 different levels (from 0.25 to 4 m) and sampled at 1 Hz. It reveals that the horizontal wind variance, the Eulerian integral scales, the frequency range of turbulence and the turbulent kinetic energy dissipation rate are affected by the surface roughness. In the vicinity of the ground surface, the horizontal wind variance logarithmically increases with height, directly in relation to the friction velocity and the roughness length scale. It was found that the time integral scale (and subsequently the length integral scale) increased with the surface roughness and decreased with the anemometer height. These variations imply some shifts in the meteorological spectral gap and some variations of the spectral peak length scale. The turbulent energy dissipation rate, affected by the soil roughness, shows a z-less stratification behaviour under stable conditions. In addition to the characterization of the studied ASL, this paper intends to show which turbulence characteristics, and under what conditions, are accessible through the cup anemometer.<br><br><b>Key words. </b>Meteorology and atmospheric dynamics (climatology, turbulence, instruments and techniques)https://www.ann-geophys.net/21/2119/2003/angeo-21-2119-2003.pdf
collection DOAJ
language English
format Article
sources DOAJ
author S. Yahaya
J. P. Frangi
D. C. Richard
spellingShingle S. Yahaya
J. P. Frangi
D. C. Richard
Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
Annales Geophysicae
author_facet S. Yahaya
J. P. Frangi
D. C. Richard
author_sort S. Yahaya
title Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
title_short Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
title_full Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
title_fullStr Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
title_full_unstemmed Turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (Northern Spain)
title_sort turbulent characteristics of a semiarid atmospheric surface layer from cup anemometers – effects of soil tillage treatment (northern spain)
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2003-10-01
description This paper deals with the characteristics of turbulent flow over two agricultural plots with various tillage treatments in a fallow, semiarid area (Central Aragon, Spain). The main dynamic characteristics of the Atmospheric Surface Layer (ASL) measured over the experimental site (friction velocity, roughness length, etc.), and energy budget, have been presented previously (Frangi and Richard, 2000). The current study is based on experimental measurements performed with cup anemometers located in the vicinity of the ground at 5 different levels (from 0.25 to 4 m) and sampled at 1 Hz. It reveals that the horizontal wind variance, the Eulerian integral scales, the frequency range of turbulence and the turbulent kinetic energy dissipation rate are affected by the surface roughness. In the vicinity of the ground surface, the horizontal wind variance logarithmically increases with height, directly in relation to the friction velocity and the roughness length scale. It was found that the time integral scale (and subsequently the length integral scale) increased with the surface roughness and decreased with the anemometer height. These variations imply some shifts in the meteorological spectral gap and some variations of the spectral peak length scale. The turbulent energy dissipation rate, affected by the soil roughness, shows a z-less stratification behaviour under stable conditions. In addition to the characterization of the studied ASL, this paper intends to show which turbulence characteristics, and under what conditions, are accessible through the cup anemometer.<br><br><b>Key words. </b>Meteorology and atmospheric dynamics (climatology, turbulence, instruments and techniques)
url https://www.ann-geophys.net/21/2119/2003/angeo-21-2119-2003.pdf
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