Oceanographers Call for Study on Impact of Floating Wind on Shelf Seas Mixing and Marine Life

(OE) While floating wind farms are seen as the next big thing in the renewable energy industry as they can be installed further from shore where the winds are stronger, oceanographers from the UK’s Bangor University are calling for new research to be done into the environmental impact of turbulence caused by tidal flow past floating deep-water wind farms and shelf sea ecosystems

The UK, which is among the world-leading countries when it comes to installed capacity – currently around 10 GW – earlier this year increased the target for offshore wind to 50 GW by 2030. Of this, 5 GW will be floating wind. Previously, the UK had a goal of building 40 GW by 2030 of which 1 GW would have been floating wind.

“New floating offshore wind turbines in the deep shelf seas have been identified as a major pathway toward achieving NetZero for the UK. The technology involved has extended growth targets – the current target to produce 50GW by 2030 is an increase of 67% on the target set just 12 months ago. But with an additional 20,000 wind turbines set to be built, we need to ensure that we’re fully aware of the positive and negative effects their presence could have on the surrounding environment,” reads a statement released by Bangor University.

Most of the world’s wind farms are conveniently located in the shallow waters near the shore. However, new offshore sites at a depth of over 50 meters are very different in nature to the shallow coastal sites that have been used so far, the statement further reads.

 A diagram illustrating the current and future types of marine wind turbines, the one in the shallowest sea has a solid 'pole' the second sits on a 'pylon-like' structure and the next two are anchored by chains to the sea bed
A diagram showing the existing and emerging offshore wind designs, including fixed monopile and jacket foundations in shallow water and floating semi-submersible and spar-buoy foundations planned for use in future deepwater developments. Credit: Bangor University

As Dr Ben Lincoln of Bangor University explains:”Our shelf seas are fully mixed during winter, but during summer months the deeper regions stratify, with a warm surface layer overlying the cooler water below. This triggers a phytoplankton bloom which can be seen from space and forms the base of the marine food chain, supporting fish, seabirds and whales. During the summer months following the spring bloom, phytoplankton growth is supported by nutrients stirred up from below by turbulence associated with wind and tides. This turbulence also mixes oxygen down to the deep water, where it is required for other key biological processes.”

New research is needed to fully understand how siting varying types of wind turbines could affect not only the seabed, but the waters, and everything they contain.

“Environmental assessments for the shallow shelf seas have focused on wildlife using or living within the affected areas. The difference with the deeper seas is that the fundamental functioning of the seas themselves could be affected,” explains Dr Lincoln.

“Turbulent mixing determines the timing and rate of the food supply on which marine ecosystem and key species rely. Flow past deep water wind farms will introduce ‘anthropogenic’ or man-made turbulence, and increase mixing. This fundamental change could lead to significant regional impacts, which must be assessed. However, impacts are not necessarily negative, with the potential to enhance productivity and offset the impact of increasing stratification due to climate change.

“There’s no doubt that this growth in renewable energy is essential to meet global 2050 Net Zero commitments. However, we urgently need a deeper understanding of the dynamics involved in placing offshore wind farms, from a single unit to large arrays, and how that will affect the functioning of our shelf sea ecosystems. This understanding will help guild the planning of new wind farms to ensure they have a positive impact on the ecosystem”.

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