If the offshore wind turbines are too numerous, they will produce less power; this should be considered when planning the farms
Credit: Photo: Nicholas Doherty via Unsplash
The expansion of wind energy in the German Bight and the Baltic Sea has accelerated enormously in recent years. The first systems went into operation in 2008. Today, wind turbines with an output of around 8,000 megawatts rotate in German waters, which corresponds to around eight nuclear power plants. But space is limited. For this reason, wind farms are sometimes built very close to one another. A team led by Dr. Naveed Akhtar from Helmholtz Zentrum Hereon has found that wind speeds at the downstream windfarm are significantly slowed down. As the researchers now write in the journal Nature Scientific Reports, this braking effect results in astonishingly large-scale low wind pattern noticeable in mean wind speeds. On average, they extend 35 to 40 kilometers – in certain weather conditions even up to 100 kilometers. The output of a neighboring wind farm can thus be reduced by 20 to 25 percent, which ultimately leads to economic consequences. If wind farms are planned close together, this wake effects need to be considered in the future.
Combination of climate and wind farm data
With their study, Naveed Akhtar, an expert in regional climate modeling, and his colleagues took a look into the future and assessed the wind characteristics for a medium-term target state of offshore expansion. They used the computer model COSMO-CLM, which is also used by weather services and which is able to resolve weather situations regionally in detail – in this case for the entire North Sea and combined it with the future wind farm characteristic – their area and the number and size of the turbines. They used the wind farm planning for the North Sea from 2015 as a basis. This contains wind farms, some of which have not yet been built.
Braking effect especially in stable weather conditions
Naveed Akhtar used the COSMO model to calculate the wind speed over the North Sea for the period from 2008 to 2017 covering a range of different weather conditions. The results clearly show that we will face a large scale pattern of reduced wind speed, which show largest extensions during stable weather conditions, typically the case in March and April. In stormy times, on the other hand – especially in November and December – the atmosphere is so mixed that the wind farm wake effects are relatively small. In order to verify the model data, the team compared the simulations with wind measurements from 2008 to 2017. They used measurements that were recorded on two research platforms in the North Sea and data from wind measurement flights that colleagues from the TU Braunschweig performed over existing wind farms. The comparison shows that the Hereon researchers are correctly simulating the wind wakes. What is special about the work is that for the first time a full ten-year period has been calculated for the entire North Sea. “Conventional flow models for analyzing wind farms have a very high spatial resolution, but only look at a wind field over a short period of time,” says Akhtar. “In addition, these cannot be used to determine how a wind farm changes the air flow over a large area.”
While the group has mainly dealt with the extent to which the wind farms influence each other in their current work, they intend to investigate in the near future what influence the reduced wind speeds have on life in the sea. Wind and waves mix the sea. This changes the salt and oxygen content of the water, its temperature and the amount of nutrients in certain water depths. Naveed Akhtar: “We would now like to find out how the reduced mixing affects the marine ecosystem.”
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