Effect of wind speed gradients on AEP in a wind farm cluster

Master Thesis (2019)
Author(s)

P.A.R. Duffy (TU Delft - Aerospace Engineering)

Contributor(s)

S.J. Watson – Mentor (TU Delft - Wind Energy)

Paul van der Laan – Mentor (Technical University of Denmark (DTU))

Alfredo Peña – Mentor (Technical University of Denmark (DTU))

Faculty
Aerospace Engineering
Copyright
© 2019 Patrick Duffy
More Info
expand_more
Publication Year
2019
Language
English
Copyright
© 2019 Patrick Duffy
Graduation Date
15-08-2019
Awarding Institution
Delft University of Technology, Technical University of Denmark, Technical University of Denmark (DTU)
Project
Rotor Design Track
Programme
European Wind Energy Masters (EWEM)
Faculty
Aerospace Engineering
Reuse Rights

Other than for strictly personal use, it is not permitted to download, forward or distribute the text or part of it, without the consent of the author(s) and/or copyright holder(s), unless the work is under an open content license such as Creative Commons.

Abstract

The engineering flow models used to estimate annual energy production (AEP) in offshore wind farm layout optimization typically assume inflow homogeneity over the model domain. This assumption lies in contrast with observations of horizontal wind speed gradients in coastal regions where many offshore wind farms are being constructed. Accounting for wind speed gradients in wind farm models may lead to reduced uncertainty in AEP estimates and reduced bias in
optimized wind farm layouts. This thesis examines whether accounting for horizontal wind speed gradients with WRF simulated wind resource inputs to engineering wake models impacts AEP prediction for a wind farm cluster in the Irish Sea by comparing results with calculation methods which assume homogeneous inflow. Analysis of a wake free two turbine case under a gradient shows that the assumption of homogeneity leads to errors with the true power which a gradient based method is able to predict. Despite this, results suggest that the overall impact of modelling wind speed gradients on AEP predictions in the Irish Sea cluster is small. Homogeneous and gradient methods using the same wind resource data predicted differences in AEP of between 0.1% and 0.75%, with most cases below 0.75%. Filtering by wind direction reveals AEP differences larger than the assumed wake model uncertainty for two sectors with inflow from land. The AEP contribution from sectors with mean wind speed gradients is limited by low frequencies and mean wind speeds. Additionally, positive and negative power differences predicted by homogeneous and gradient methods were found to balance over the year.

Files

Final_Thesis_Duffy.pdf
(pdf | 7.15 Mb)
License info not available