A NUMERICAL STUDY OF WIND SPEED-UP OVER HYDROELECTRIC RESERVOIRS OF THE SOUTHEAST REGION OF BRAZIL

Authors

  • Cláudio de Castro Pellegrini Universidade Federal de São João del-Rei (UFSJ), São João del-Rei, MG
  • Almilson Vilhena Leite Neto Universidade Federal de São João del-Rei (UFSJ), São João del-Rei, MG
  • João Victor Burgareli de Assis Universidade Federal de São João del-Rei (UFSJ), São João del-Rei, MG
  • Arcilan Trevenzoli Assireu Universidade Federal de Itajubá, Itajubá, MG

DOI:

https://doi.org/10.5902/2179460X20170

Keywords:

Wind potential. Mesoscale modeling. WRF model. Hydroelectric reservoirs.

Abstract

Brazil has a large hydric potential explored in many ways, especially for electrical generation. However there is a lack of studies about the wind acceleration a converge over the reservoir, affected by the surrounding topography and the low roughness of the water surface. In this work an evaluation of the phenomenon is performed thought observed data and numerical simulation using the WRF atmospheric model. The selected reservoirs are located in the Brazilian south-east region, and both have operating infrastructure of transmission. In view of that, we have tried to understand the influence of the joint reservoir-topography over the wind behavior. It was verified that in the Itumbiara reservoir (Goias State), the wind experiences acceleration with both cross and aligned wind with respect to the reservoir branches. Otherwise, the Tres Marias reservoir (State of Minas Gerais) shows that in the case of non-aligned wind the reservoir has not a significant influence over wind speed. It is concluded that for both reservoirs wind speed-ups are verified, caused by the joint reservoir- topography influence, that becomes more evident with speeds over 3.0 m/s (10 m over the ground) a velocity matching modern wind turbines cut out speed.

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References

Assireu, A., Pimenta, F., Souza, V. (2011). As-sessment of wind power potential of hydroe-lectric reservoirs. Em: Energy resources: de-velopment, distribution and exploitation, pp. 1-28.

Assireu, A., Pellegrini, C.C., Pimenta, F. (2013). Intensificação do vento devido a influências do relevo: evidências a partir de modelos numéricos e medidas in situ. Em: X Workshop Brasileiro. Micrometeorologia. UFSM, Santa Maria, RS.

Bullard, J. E.; Wiggs, G.F.S.; Nahs, D. J. (2000). Experimental study of wind directional vari-ability in the vicinity of a model valley. Em: Geomorphology, 35, 127-143.

INMET, Normas Climatológicas do Brasil (1961-1990). Ins. Nac. Meteorologia. Disponível em: http://www.inmet.gov.br/portal/index.php?r=clima/normaisClimatologicas. Acesso: 29 de abril de 2013.

Kaimal, J. C. and Finnigan, J. J. (1994). Atmos-pheric Boundary Layer Flows: Their Structure And Measurement. Oxford Univ. Press, New York, 289 pp.

Lange, B., Larsen, S., Hojstrup, J., Barthelmie, R. (2004). Importance of thermal effects and sea surface roughness for offshore wind resource assessment. Em: Journal of Wind Engineering, 92, 959-988.

Manwell, J. F.; McGowan J. G. and Rogers, A. L. Wind energy explained, John Willey and Sons, West Sussex, England, 590 pp., 2002.

Peña, A., Gryning, S.E. (2008). Charnock’s roughness length model and non-dimensional wind profiles over the sea. Em: Bound.-Layer Meteor., 128(2), 191-203.

Peña, A., Gryning, S.E., Hasager, C.B. (2009). Measurements and modeling of the wind speed profile in the Marine Atmospheric Boundary Layer. Em: Bound.-Layer Meteor., 129(3), 479-495.

Sathe, A., Gryning, S.E., Peña, A. (2011). Com-parison of the atmospheric stability and wind profiles at two wind farm sites over a long marine fetch in the North Sea. Em: Wind E-nergy, 14(6), 767-780.

Published

2016-07-20

How to Cite

Pellegrini, C. de C., Leite Neto, A. V., Assis, J. V. B. de, & Assireu, A. T. (2016). A NUMERICAL STUDY OF WIND SPEED-UP OVER HYDROELECTRIC RESERVOIRS OF THE SOUTHEAST REGION OF BRAZIL. Ciência E Natura, 38, 197–203. https://doi.org/10.5902/2179460X20170