scispace - formally typeset
M

M. E. Harrison

Researcher at University of Southampton

Publications -  5
Citations -  409

M. E. Harrison is an academic researcher from University of Southampton. The author has contributed to research in topics: Wake & Reynolds-averaged Navier–Stokes equations. The author has an hindex of 4, co-authored 5 publications receiving 380 citations. Previous affiliations of M. E. Harrison include Bristol and Bath Science Park.

Papers
More filters
Journal ArticleDOI

Comparison between CFD simulations and experiments for predicting the far wake of horizontal axis tidal turbines

TL;DR: In this paper, the authors compare the characteristics of the wake of an actuator disc, modelled using a steady solution to the Reynolds-averaged Navier-Stokes (RANS) simulated equations, with the k-ω shear stress transport (SST) turbulence model, to experimental data measured behind discs of various porosities.
Journal ArticleDOI

Accuracy of the actuator disc-RANS approach for predicting the performance and wake of tidal turbines.

TL;DR: Comparisons show that the model is accurate and can predict up to 94 per cent of the variation in the experimental velocity data measured on the centreline of the wake, demonstrating that the actuator disc-RANS model is an accurate approach for modelling a turbine wake, and a conservative approach to predict performance and loads.
Proceedings ArticleDOI

A blade element actuator disc approach applied to tidal stream turbines

TL;DR: In this article, a computationally efficient method for predicting the performance of an array of turbine arrays is presented, which is similar to BEM theory but can predict the flow field as well as the rotor performance.

The sensitivity of actuator-disc RANS simulations to turbulence length scale assumptions

TL;DR: In this article, the authors investigated the effects of using different length scales on the development of a flow in a circulating water channel and found that the best agreement is achieved with a length scale of one third the channel depth.