Evaluation of two wind flow models for wind resource assessment for a site

Vilas Warudkar; Pramod Sharma; Siraj Ahmed

doi:10.1051/e3sconf/202016705001

All issues

Volume 167 (2020)

E3S Web Conf., 167 (2020) 05001

References

Open Access

Issue		E3S Web Conf. Volume 167, 2020 2020 11^th International Conference on Environmental Science and Development (ICESD 2020)


Article Number		05001
Number of page(s)		4
Section		Renewable Energy
DOI		https://doi.org/10.1051/e3sconf/202016705001
Published online		24 April 2020

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[1] Troen I, Petersen EL. European wind atlas. Report from the Risø National Laboratory, Roskilde, Denmark, 1989. [Google Scholar]

[2] Troen I. A High-resolution spectral model for flow in complex terrain. Proceedings from the 9th Symposium on Turbulence and Diffusion, Roskilde, Denmark, 1990. [Google Scholar]

[3] Beljaars ACM, Walmsley JL, Taylor PA. A mixed spectral finite-difference model for neutrally stratified boundary-layer flow over roughness changes and topography. Boundary-Layer Meteorology. 1987; 38: 273–303. [Google Scholar]

[4] Jackson P, Hunt JCR. Turbulent wind flow over a low hill. Quarterly Journal of Royal Meteorological Society. 1975;101: 929–955. [CrossRef] [Google Scholar]

[5] Bitsuamlak GT, Stathopoulos T, Bédard C. Numerical evaluation of wind flow over complex terrain: a review. Journal of Aerospace Engineering. (8) 2004; 17: 135–145. [Google Scholar]

[6] Mortensen NG, Bowen AJ, Antoniou I. Improving WAsP predictions in (too) complex terrain. Proceedings from EWEC, Brussels, Belgium, 2008. [Google Scholar]

[7] Brower. Wind resource assessment: a practical guide to developing a wind project. Wiley editions: New York, 2012; 280. [Google Scholar]

[8] Yamada T. Simulations of nocturnal drainage flows by a q2l turbulence closure model. Journal of Atmospheric Sciences. 1983; 40: 91–106. [CrossRef] [Google Scholar]

[9] Arritt RW. The effect of water surface boundary layers. Boundary-Layer Meteorology. 1987; 40: 101–125. [Google Scholar]