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Neill simon day2_session_4_b_marine_evidence_swansea_neill
1. Ocean renewable energy β
resource & impacts
Simon Neill*, Matt Lewis, Peter Robins
School of Ocean Sciences,
Bangor University, UK
*s.p.neill@bangor.ac.uk
DrSPNeill
4. 3D model of the Irish Sea:
resolution 1/240Β° x
1/404Β° ~278m
10 depth levels
Peak current
speed (m/s)
Lewis et al. (2015)
5. Co-tidal chart
5
β’ Co-tidal lines join locations which
are in phase (i.e. HW occurs at the
same time)
β’ Co-amplitude lines join locations
that have the same tidal amplitude
(which is half of the tidal range)
M2
Neill & Scourse (2010)
7. Impact of energy extraction on bed shear
stress/sediment transport
β’ Bed shear stress is a function
of U2.
β’ Small changes in the tidal
currents could lead to large
changes in the corresponding
bed shear stress.
β’ Transport of sediments is
proportional to an even higher
power of velocity than bed
shear stress, e.g. U3. Neill et al.
(2009)
U2
U
17. Tidal-stream energy extraction
How do TEC arrays affect:
β Suspended sediment?
β Formation of sand banks?
β Net sediment fluxes?
Is the impact significant relative to natural
intra-seasonal and inter-annual variations?
TEC array simulations:
β’ Turbines induce drag force on flow
πΉπΉπ₯π₯ = βπΆπΆππ
ππ
ππππππππ
ππππππ ππ
β’ TEC array rated power modelled:
β’ 10, 50, 100, 300, 500 MW
Robins et al. (2014)
19. Conclusions
β’ Sediment present even in regions of very strong
tidal flow
β’ Turbines could lead to a local increase in bed
shear stress
β 3D modelling required
β’ Impact significant for large scale extraction, e.g. >
100 MW
β’ Impact needs to be assessed against natural
variability
β’ Validation & tuning of sediment transport and
energy extraction required