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In the atmospheric boundary layer, the Coriolis force associated with the Earth’s rotation induces a spanwise wind shear in addition to the wall-normal one leading to a continuous change in wind direction with height. The spanwise wind shear in directionally sheared inflow has a significant impact on the formation and development of wind-turbine wakes. The present work aims to provide an analytical framework for predicting wind turbine wakes in directionally varying wind shears.
Fernando Porté Agel, Peter Andreas Brugger, Corey Dean Markfort
Jian Wang, Julia Schmale, Andrea Baccarini, Ivo Fabio Beck, Hélène Paule Angot, Lubna Dada