Here's a picture of the FINO3 platform:
Scientists of the Geesthacht GKSS Research Centre have developed a radar system with which it is possible to study the behaviour of sea waves. This technology will be used immediately on the North Sea on the FINO3 research platform in order to determine the interactions between offshore wind power machines and swells.
The location of the FINO3 research platforms, the "Dan Tysk" sand bank, is located approximately 80 kilometres to the west of Sylt where up to 80 wind power plants will be located in just a few years. FINO3 is used by researchers to estimate the environmental consequences and technical risks of offshore wind energy parks. Changes in the sea swell are also of great interest in addition to the observations of bird migration or the measurement of lightening frequencies on the sea.
To determine how much of an effect large waves and what is known as 'breakers' have on wind power plants and to what extent the structures can change the surrounding swell, the coastal researchers of the Geesthacht GKSS Research Centre installed a Doppler radar approximately 50 metres above sea level on the FINO3 lattice mast.
"With our radar, we can even track the individual waves for the first time", writes Dr. Freidwart Ziemer, GKSS Department Manager of Radar Hydrology, the unique part of the project. For several years, Ziemer and his team have studied the swell and the behaviour of large breakers. The information is transmitted by FINO3 to Geesthacht via satellite.
The frequency of large breakers and the force which creates the steep giant waves are of particular interest not only to researchers but also the designers and operators of offshore wind power plants or oil platforms.
Each individual wind rotor creates turbulent air flows in its "tow" and periodical movements, which can have an effect on other structures. This can result in undesired or even dangerous vibrations. If there is an interaction between the waves and the individual wind power plants, this can result in interferences. This means in a wave field which is harmless without a windmill park, single, very high waves can be created by these interferences which could possibly have a critical effect on these plants.
"I am sure that we will soon be able to better assess the swells and the force of the breakers," says Friedwart Ziemer. This means that the breaker behaviour could be taken into account better in planning and the stability of the systems can be more predictable.
I have never heard of this thing. Some of the GKSS wave people I know do not seem to connected to this project. I don't know how much research they wish to do in the project. I do think they have strong potential for collecting great data sets for fruitful research, because all those wealth of data they can collect will be truly exciting. I'm keeping my eyes widely open for their continued progress and success.