Preprints
https://doi.org/10.5194/wes-2025-239
https://doi.org/10.5194/wes-2025-239
20 Nov 2025
 | 20 Nov 2025
Status: this preprint is currently under review for the journal WES.

Wind profiles and low-level jet structures over the coastal waters of Japan

Kauzutaka Goto, Takanori Uchida, and Keisuke Nakao

Abstract. Accurate characterization of coastal wind conditions is essential for offshore wind energy development; however, atmospheric structures in Japan's nearshore regions remain poorly understood. This study analyzed year-long vertical light detection and ranging (LiDAR) observations at closely located onshore and offshore sites along the Aomori coast to clarify the differences in wind profiles and their seasonal and directional dependence. Offshore wind speeds showed strong correlations (r >0.8) with onshore data, indicating that, although direct substitution is inappropriate, onshore observations can effectively serve as reference data for offshore extrapolation when using the measure–correlate–predict (MCP) method. Low-level jets (LLJs) were frequently observed in spring and summer, particularly when wind directions aligned with the coastline, with occurrence rates ≥20 % higher than in other seasons. Case analyses revealed that diurnal transitions associated with land–sea breeze circulation modulate vertical mixing and surface friction, promoting the development of LLJs. These results advance our understanding of nearshore boundary-layer dynamics and provide a basis for improving assessments of offshore wind resources, turbine designs, and LLJ forecasting strategies.

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Kauzutaka Goto, Takanori Uchida, and Keisuke Nakao

Status: open (until 18 Dec 2025)

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Kauzutaka Goto, Takanori Uchida, and Keisuke Nakao
Kauzutaka Goto, Takanori Uchida, and Keisuke Nakao

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Short summary
This study investigated coastal wind conditions in Japan using year-long light detection and ranging observations from onshore and offshore sites, 1.6 km apart. The wind speed profiles differed significantly. Low-level jets (LLJs) occurred more frequently in specific seasons and wind directions, and their timing varied with direction. These findings indicate a strong link between land-sea breeze circulation and LLJ formation and demonstrate the need for further Japan-specific evaluations.
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