Journal
ENERGIES
Volume 15, Issue 7, Pages -Publisher
MDPI
DOI: 10.3390/en15072319
Keywords
remote sensing; SODAR; LIDAR; micrometeorology tower; marine boundary layer; sea-land transition; wind speed profile; wind energy; solar energy
Categories
Funding
- Equatorial Energia
- Gera Maranhao under Brazilian Electricity Regulatory Agency (ANEEL) RD Program [PD-00037-0042/2020]
- National Council for Scientific and Technological Development of Brazil (CNPq)
- Foundation for Support to Research and Scientific and Technological Development of Maranhao (FAPEMA)
- Coordination for the Improvement of Higher Education Personnel (CAPES)
- National Institute of Science & Technology in Ocean and Fluvial Energies (INEOF)
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The EOSOLAR project aims to investigate the structure of the atmospheric boundary layer in an equatorial coastal zone using ground-based remote sensing instruments and micrometeorological towers. This paper describes the study area, methodology, and instrumentation of the project, and presents results of the first field campaign and instrument validation.
The EOSOLAR project was designed to investigate the structure of the atmospheric boundary layer in an equatorial coastal zone, where the discontinuity of surface conditions induces non-stationarity gradients of wind speeds and the development of internal boundary layers. The proposed methodology considers several aspects of the sea-land transition meteorology that are essential for precisely estimating wind-solar energy potential and assessment of structural loads on wind turbines. Infrared (LIDAR) and acoustic (SODAR) ground-based remote sensing instruments and micrometeorological towers were installed in a near-shore equatorial area of northeast Brazil, in order to provide a comprehensive view of meteorological processes. This paper reports a description of the project study area, methodology, and instrumentation used. Details of instruments configurations, a validation of micrometeorology towers, and a comparison between the LIDAR and SODAR are presented. Results of the first field campaign measuring the coastal flow, integrating the micrometeorological tower and LIDAR observations are described.
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