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Modelling Changes to Physical Environmental Impacts due to Wave Energy Array Layouts Helen Smith, Ian Ashton EIMR 2014, Stornoway 20.05.2014 Overview 1. Context: The EBAO project 2. Theoretical modelling study 3. Case study for EMEC 4.


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20.05.2014

Helen Smith, Ian Ashton

EIMR 2014, Stornoway

Modelling Changes to Physical Environmental Impacts due to Wave Energy Array Layouts

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Overview

1. Context: The EBAO project 2. Theoretical modelling study 3. Case study for EMEC 4. Conclusions and future work

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EBAO

“Optimising Array Form for Energy Extraction and Environmental Benefit”

Scenario A: Constrained channel Tidal Scenario B: Sea area between Tidal mainland and island Scenario C: Inshore site Wave, Tidal Scenario D: Offshore site Offshore wind

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Theoretical model

  • 3 array scenarios
  • Grid:
  • Parallel depth contours
  • Real bathymetry (Orkney)
  • Deepest device located at 60m depth
  • 2 sea states – average and large
  • 5 wind scenarios
  • All modelling using SWAN spectral wave model
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Theoretical model – Scenario1

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Theoretical model – Scenario 2

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Theoretical model – Scenario 3

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Wind scenarios Following: 5ms-1, 10ms-1, 20ms-1 Opposing: 10ms-1 Cross: 10ms-1

Theoretical model

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  • SWAN spectral wave model
  • Devices represented as 50m partially transmitting barriers
  • Frequency-dependent energy absorption
  • Limitations of SWAN?

TrCoeff = HsT/HsI

Theoretical model

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Output

200m 1000m 5000m 10000m Shore Centre

Theoretical model

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Sea state 1, no wind

Theoretical model - results

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  • Increasing the number of devices increases the impact
  • Clusters of devices with corridors lessen impact closer

to devices, but this becomes negligible by the shoreline

  • Impact decreases with increasing following or cross

wind

  • Impact increases with opposing wind
  • Impact increases at shoreline for steeper seabed
  • Impact slightly higher for larger sea state

Theoretical model - summary

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EMEC case study

  • 4
  • 3.6
  • 3.2
  • 2.8
  • 2.4
  • 2

58 58.4 58.8 59.2 59.6 60

  • Run over full

year (2005)

  • Input data from

EMEC hindcast

  • Same 3

scenarios modelled

  • Output at three

~10m depth locations

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Location 1

EMEC case study

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Sea state corresponding to ‘small’ sea state, 20/3/05 15:00: Hs = 1.56m, Tm = 5.3s, D = 275°

EMEC case study

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Sea state corresponding to ‘small’ sea state, 20/3/05 15:00: Hs = 1.56m, Tm = 5.3s, D = 275°

EMEC case study

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Sea state corresponding to ‘small’ sea state, 20/3/05 15:00: Hs = 1.56m, Tm = 5.3s, D = 275°

EMEC case study

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Conclusions

  • Array layout is important for near-field effects, less so

for the far-field

  • Local wind and wave conditions more influential on the

scale of the impact

  • Next stage is to examine how these impacts affect

wider physical and ecological scenarios

  • Further work ongoing to develop the capability of

spectral wave models to prediction such impacts – need validation!

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Thank you!

h.c.m.smith@exeter.ac.uk i.g.c.ashton@exeter.ac.uk