Introducing a High Resolution Atlas of U.S. Offshore Wind Profiles

The U.S. offshore wind energy industry is a growing endeavor. As such, stakeholders in this industry need information about winds from the ocean surface up to wind turbine hub heights of ~100m to 200m. Accurate wind speed observations within the rotor layer of wind turbines are scarce, with sparsely spaced coastal meteorological towers, as well as site-specific sodars and lidars, serving the only sources of information. 

 

Leveraging satellite-based products, with their high spatiotemporal coverage, and machine learning methods, offers a way of developing detailed wind speed profile gridded datasets for practical use by stakeholders. In a paper published in the journal Wind Energy Science, ESSIC/CISESS Scientists James Frech, Paige Lavin, and colleagues use random forest regression (RFR), a machine-learning technique, to accurately estimate offshore wind speed profiles on a 0.25° grid at a six-hour resolution from 1987 to the present. 

Figure. Seasonal climatologies (1987–2022) for wind profiles extrapolated from NOAAOffshoreWindProfiles-USA (unit: m s-1) at (a-d) 20, (e-h) 100, and (i-l) 200 m. DJF: December, January, February; MAM: March, April, May; JJA: June, July, August; SON: September, October, November.
Figure. Seasonal climatologies (1987–2022) for wind profiles extrapolated from NOAAOffshoreWindProfiles-USA (unit: m s-1) at (a-d) 20, (e-h) 100, and (i-l) 200 m. DJF: December, January, February; MAM: March, April, May; JJA: June, July, August; SON: September, October, November.

Their methodology is applicable to the coastal regions of the contiguous U.S. and Hawai‘i and uses satellite-derived surface wind speeds from the NOAA NCEI Blended Seawinds version 2.0 product as input. They report that their RFR model has the advantage of requiring fewer input variables and outperforms traditional methods when it comes to estimating wind speeds at wind turbine hub heights in the presence of high vertical wind shear and low-level jets (LLJs). Additionally, previous studies using RFR to estimate wind speeds were limited to smaller areas and thereby of limited utility, while this RFR model is able to perform robustly over a large region.

 

One important focus of future work will be to predict the wind speed gradient inversion of an LLJ, a current limitation of their model. The final product generated by the model, NOAAOffshoreWindProfiles-USA, will be archived with NCEI for public access.

This article was put together by the CISESS coordinators based on scientist input.

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Debra Baker

Debra Baker is the Coordinator for the Cooperative Institute for Satellite Earth System Studies (CISESS) at the University of Maryland. She received her M.S. in atmospheric science from the University of Maryland, College Park. Before joining ESSIC in 2013, she worked on air quality issues at the Maryland Department of the Environment. Debra also has a law degree from Harvard Law School.

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Kate Cooney

Katherine Cooney is a part-time faculty assistant at the Cooperative Institute for Satellite Earth System Studies (CISESS). Kate received a B.S. in environmental science and policy from the University of Maryland (UMD), College Park. She later earned a M.S. in geology from UMD, while investigating the isotopic fractionation of precipitation nitrate under the guidance of Distinguished University Professor James Farquhar. After graduation, she worked as an air-quality specialist at the Mid Atlantic Regional Air Management Association in Baltimore, Maryland. While her family was stationed in Tokyo, Japan, she dedicated her time serving military families and the local community. She is grateful for the opportunity to return to earth system studies, supporting the CISESS Business Office and assisting the CISESS Coordinator Deb Baker since January 2021.

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Maureen Cribb