As US’ first offshore wind farm takes root, study indicates wind may be more powerful, turbulent than expected

University of Delaware researchers report in a new study that offshore wind may be more powerful, yet more turbulent than expected in the North Eastern United States.
The findings, published in a paper in theJournal of Geophysical Research: Atmospheres, could have important implications for the future development of offshore wind farms in the U.S., including the assessment of how much wind power can be produced, what type of turbines should be used, how many turbines should be installed and the spacing between each.
The study, led by Cristina Archer at UD and Brian Colle at Stony Brook University, analyzed historical data from 2003-2011 at the Cape Wind tower located near the center of Nantucket Sound off the coast of Martha’s Vineyard, Massachusetts, and collected complementary data at the same location in 2013-2014.
Co-authors on the paper, titled “On the predominance of unstable atmospheric conditions in the marine boundary layer offshore of the U.S. northeastern coast,” include UD professors Dana Veron and Fabrice Veron, and Matthew Sienkiewicz from Stony Brook.
The paper’s main finding is that atmospheric conditions around Cape Wind are predominantly turbulent, or unstable, which is in stark contrast to prevailing data from European offshore wind farms in the Baltic Sea and the North Sea. European studies of offshore wind document that atmospheric conditions there are predominantly neutral– meaning neither too windy nor too still, but somewhere in the middle, with unstable wind conditions occurring only 20 percent of the time.
“By contrast, our study found that wind conditions at Cape Wind are unstable between 40 and 80 percent of the time, depending on season and time of day,” explains Archer, an associate professor in the College of Earth, Ocean, and Environment’s School of Marine Science and Policy and Department of Geography and a governing member of the Center for Carbon-free Power Integration.
Stable, unstable and neutral
Explaining how wind can be stable, unstable or neutral is a tricky business, Archer says. When the atmosphere is stable, winds are smooth and consistent (think of when a pilot tells airline passengers to sit back and enjoy the ride because the weather is clear all the way to their destination).
When the atmosphere is unstable, it is similar to turbulence experienced by airline passengers during a flight — the wind is choppy and causes high winds from above and slow winds from below to crash into each other and mix together, causing a bumpy and unpredictable ride for the air current.
Neutral conditions hover in the middle, with an average amount of turbulence and wind speed variation.
“The advantage of these turbulent conditions is that, at the level of the turbines, these bumps bring high wind down from the upper atmosphere where it is typically windier. This means extra wind power, but that extra power comes at a cost: the cost of more stress on the turbine’s blades,” explains Archer.
An expert in designing offshore wind farms, Archer says the findings may have implication on how future offshore wind farms in the region are designed.
“If you have increased turbulence, you’re going to design a different farm, especially with regard to turbine selection and spacing. And guess what? Even the wind turbine manufacturing standards are based on the assumption of neutral stability,” Archer says.
Is something special going on in the North East?
No measurements exist of wind and turbulence around an offshore wind turbine’s rotor blades in the ocean in the U.S., because until now, none have existed. The first U.S. offshore wind farm is currently under construction at Block Island, off the coast of Rhode Island.
Instead, this type of data has been estimated based on either numerical simulations or using available buoy data to infer what the conditions would be at the height of the wind turbine’s rotor blades. But wind data measurements from 2003-2009 at the Cape Wind Tower, a multi-level tower with sensors positioned approximately 65 feet, 131 feet and 196 feet in height, have shown that the Cape Cod region’s atmospheric conditions are generally unstable. Neutral conditions only occur approximately 20 percent of the time.
In 2013 and 2014, with funding from the U.S. Department of Energy, the UD-led research team launched a campaign they coined IMPOWR, Improving the Modeling and Prediction of Offshore Wind Power Resources, to validate the Cape Wind tower findings with additional measurements.
The IMPOWR researchers flew a plane around Cape Wind 19 times over two summers, above and around the tower, and measured wind, temperature and humidity during various weather conditions. They also installed new wind and wave sensors on the Cape Wind platform.
Combined with buoy data from just above the water’s surface and with the historical data from Cape Wind, the IMPOWR field data painted a surprising and yet consistent picture of the area’s wind resources.
“We get the same message whether we look at the turbulence from the flights or from the sonic anemometers on the tower, or whether we consider the wind speed data alone. The marine atmosphere is more likely to be unstable than neutral. Having three separate pieces of evidence that support the same finding allows us to be confident that there is something special going on,” she says.
Wind direction also plays a role in whether the wind is smooth or turbulent. When the wind comes from the southwest, the data show that wind tends to be more stable and to increase in speed from the bottom to the top of the rotor blades. But when the wind comes from the north, northwest or offshore, it is more likely to be unstable and to have a relatively uniform speed across the turbine rotor, Archer says.
Further study is needed to understand whether this phenomenon is localized in the Cape Cod area, along the East Coast in general, or present throughout the U.S., since other offshore wind installations on the East Coast are planned for Maryland, New Jersey and Massachusetts.
“It’s important to ensure that science doesn’t underestimate the possible wind resources,” Archer says. “Now that we know what is happening in Cape Cod, we have more work to do to determine whether it exists anywhere else or whether it is unique to this region.”
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“Is something special going on in the North East?”
Yes. Assumptions were made and not validated.
Pretty obvious that offshore winds will be stronger. You get Javier Stokes at the surface boundary, voila, turbulence.
Nullschool gives valuable lessons of relative wind strengths ocean vs land:
Why do you re-fill a water pistol when it runs out of water?
Because there is little energy in displaced air, whereas there is useful energy in displaced water.
There is little energy to be harvested from the wind. It is also variable and above all unpredictable. These facts, coupled with the fact that there is presently no practical means of storing energy, would tell any engineer that this is not an energy source capable of powering forward the 21st century. There is a reason why our forefathers abandoned windmills in the 18th and 19th centuries, and sail power in the 19th and 20th century.
The way to the future is not to go backwards to the past.
Too pre-post-modern. Don’t you know the climate white elephant needs to be built first, and the basic information on why it’s an obvious white elephant should come later? Prudent forethought is so last century.
Some video to share with your favorite wind-energy fan:
Oh the schadenfreude…
“It’s important to ensure that science doesn’t underestimate the possible wind resources,”
I think this would be more appropriate: “It’s important to ensure that science doesn’t overestimate the possible wind resources”
They should have consulted yachtsmen first. Any yachtsman would have told you that the wind is ALWAYS more unstable around a headland, and Cape Wind sounds as if it is a headland.
I guess near on four centuries worth of seafaring sailing ship’s logs of conditions in the exact area weren’t available for inclusion in the report.
Who cares? As long as Big Wind makes their dough, that’s what matters. Cape Wind was doomed from the start because of NIMBY politics. Opponents are nothing if not rank hypocrites. They love “green” energy, just not where they might have to look at it.
Interesting photo of the downstream conditions from a windmill. It is the only one that verifies of the weather modifications downstream. That’s what I complain about. There are no studies of the downstream areas. Unlike windbreaks, trees in a row, does this help the local area, or create problems. Does the turbulence change the local weather? How about, further downstream, or, the upstream pooling effect? If you block the flow here, does the wind blow heavier there? Man-made global warming created by ducting the winds?
Who pays for a damaged Cape Wind? The funders of the Big Dig (the rest of us) want to know.
Sounds like a pre-excuse for when the off shore wind farm doesn’t pan out like they thought.
I’m shocked, shocked, to learn that the air not only moves, but moves at velocities and directions beyond predictability. (Between ‘shocks’ I’m enjoying some first-rate commentary, thanks.)
They need to act fast. Pretty soon there will be no more Climate Ca$h, and the wind fakeindustry will fold like a cheap suit.
So basically a wind farm would generate 11% of the nameplate rating instead of 10%.
A refresher on the facts of offshore wind power in the US:
1) Total potential for installed power: 900 GW ( Per the U.S. Department of Interior, Mineral Mining Service, MMS, in their January 2009 “Draft Proposed Outer Continental Shelf Oil and Gas Leasing Program 2010 – 2015,” )
The MMS stated:
“The U.S. Department of Energy (DOE) estimates that more than 900,000 megawatts (900 GW), close to the total current installed U.S. electrical capacity, of potential wind energy exists off the coasts of the United States, often near major population centers, where energy costs are high and land-based wind development opportunities are limited. Slightly more than half of the country’s identified offshore wind potential is located off the New England and Mid-Atlantic Coasts, where water depths generally deepen gradually with distance from the shore. Development of offshore wind energy technologies has the potential to provide up to 70,000 MW of domestic generating capacity to the nation’s electric grid by 2025.”
2) Costs for wind turbines offshore are higher than onshore, but will steadily decline as sizes increase and more units are installed.
3) Average wind speed is higher offshore, providing more output per turbine.
4) Improved technology has been developed (or is under development) by US Sandia National Laboratory, to allow offshore turbines to continue operating in gusty or very strong winds instead of cutting out to avoid damage. The new turbine is HAWT with blades downwind of the tower, and importantly, flexible blades that bend in the wind.
see http://energy.gov/articles/enormous-blades-offshore-energy
5) Energy storage via MIT underwater spheres allows wind power to be sent to shore on demand and in load-following mode. Net energy loss is approximately 20 percent.
6) US wind energy map shows the location and strength of offshore wind – http://apps2.eere.energy.gov/wind/windexchange/windmaps/offshore.asp
Roger,
What are you talking about regarding battery storage? Where? What type? My solar system would not have allowed by to tie to the grid had we installed batteries as I wished.
The last I read, Governor Moonbeam was demanding grid scale storage, but so far nothing is on the close horizon. Has there been a break through?
Thanks,
pbh
” aging US nuclear plants, 99 of them at present”
Since nuclear is an important part of the US power supply, aging is an important topic that is being addressed by the nuclear industry. We have already figured out how to make them last 60 years and are working on 80 years.
Of course wind turbines and solar panels are also aging. I do not think storage will be needed because of the failure rate with time.
“The coal exhaustion problem is real, and imminent in the US. ”
Yes and no. Running out of fossil fuels is not imminent when considering the life span of human or wind turbines. A good argument to wait to build wind farms until they are needed.
“No measurements exist of wind and turbulence around an offshore wind turbine’s rotor blades in the ocean in the U.S., because until now, none have existed.”
— How embarrassing. Maybe Mrs Jennings 4th grade science class can offer them all some suggestions for improving things.
I’m mostly curious about how nor’easters and icing will impact Deepwater Wind than I am about wind flow. However, a query from an Email list I’m on inspired me to hunt down the paper an take a closer look. The paper is available at http://www.windaction.org/posts/45573-on-the-predominance-of-unstable-atmospheric-conditions-in-the-marine-boundary-layer-offshore-of-the-u-s-northeastern-coast Not firewalled!
The paper uses data from low level airplane flights and the Cape Wind Met (Meteorological) tower, which was not as tall as the planned turbines. The paper refers to instruments at 20, 41, and 60 meters above MLLW (Mean Lower Low Water, a term I haven’t encountered before), the Deepwater wind turbines are said to be 270 feet (82m or so) tall, but that has to be the tower height, and even that’s too low.
https://www.gerenewableenergy.com/content/dam/gepower-renewables/global/en_US/documents/haliade-offshore-wind-turbine.pdf says “Hub height 100 m (or site-specific)” and “Rotor diameter 150.95m”. That means the blade tips will be shuttling between 25m and 175m, way in excess of the Cape Wind Met tower. BTW, these are 6 MW turbines with blade lengths 50% longer than any land based turbine I’m familiar with.
I imagine the Cape Wind folks figured their Met tower would cover the boundary zone over the rotor’s swept area and that air flow would be steady above the boundary zone.
The paper says that the air flow is more complex than that. The paper looks at data recorded from an airplane at flight levels 30 – 90 meters, so those are below the nacelle too!
All in all, I really don’t know what the implications are from this. A steady, stable air flow will have wind sheer, with significantly lower wind speed at the bottom of the rotor than at the top. An unstable air flow has much less sheer, but will have quite a bit of random motion, left, right, forward, backward and even up and down. Either way they’ll have some interesting forces, they may have more trouble dealing with the random, turbulent wind.