19th Symposium on Boundary Layers and Turbulence


The offshore wind resource and boundary layer structure

Jeffrey M. Freedman, AWS Truewind LLC, Albany, NY; and C. Alonge and J. Manobianco

Coastal and offshore locales are favored regions for wind power utilization because of the generally high wind resource, proximity to major load centers, and existing transmission infrastructure. However, because of the dearth of long-term high quality observations available over the offshore waters, comparatively little is known about the three-dimensional structure of the lowest 200 m of the marine boundary layer, especially as it relates to the determination of the wind resource and turbulence effects within, above, and below the rotor plane. Recent field observations and modeling studies have shown the existence of low-level jets, or sheet-like structures, just offshore of the mid-Atlantic and northeastern U.S. coastal regions, prime areas for the development of wind power production facilities. These structures feature wind speed maxima between 70 and 120 m above the surface (Figure 1), well within the typical rotor plane of the larger wind turbines proposed for the offshore waters. Therefore, the purpose of this presentation is to show, through modeling studies and recent field observations, the spatial and temporal characteristics of the LLJs, their climatology, and their potential effect on wind resource assessment campaigns, turbine design, and load matching.

wrf recordingRecorded presentation

Session 3B, Observations and Modeling Related to Renewable Energy Applications III
Tuesday, 3 August 2010, 3:30 PM-4:45 PM, Torrey's Peak III & IV

Previous paper  Next paper

Browse or search entire meeting

AMS Home Page