Remote Sensing | |
Atmospheric Transmittance Model Validation for CSP Tower Plants | |
Luis Zarzalejo1  Stefan Wilbert2  Florian Wiesinger2  Natalie Hanrieder2  Abdellatif Ghennioui3  Ahmed Alami Merrouni3  Alexander Schade4  Manajit Sengupta5  | |
[1] Centro de Investigaciones Energéticas, Medioambientales y Tecnológicas (CIEMAT), División de Energías Renovables. Avda. Complutense 40, 28040 Madrid, Spain;German Aerospace Center (DLR), Institute of Solar Research, Plataforma Solar de Almería (PSA), Ctra. de Senés s/n km 4, Apartado 39, 04200 Tabernas, Spain;Institut de Recherche, Energie Solaire et Energies Nouvelles (IRESEN), Green Energy Park, Km 2 Route Régionale R206, Benguerir 43152, Morocco;Institute of Physics and Meteorology, University Hohenheim, 70593 Stuttgart, Germany;National Renewable Energy Laboratory, 1617 Cole Blvd, Golden, CO 80401, USA; | |
关键词: atmospheric extinction; attenuation loss; transmittance model; central receiver; solar resource assessment; CSP; | |
DOI : 10.3390/rs11091083 | |
来源: DOAJ |
【 摘 要 】
In yield analysis and plant design of concentrated solar power (CSP) tower plants, increased uncertainties are caused by the mostly unknown solar attenuation between the concentrating heliostat field and the receiver on top of the tower. This attenuation is caused mainly by aerosol particles and water vapor. Various on-site measurement methods of atmospheric extinction in solar tower plants have been developed during recent years, but during resource assessment for distinct tower plant projects in-situ measurement data sets are typically not available. To overcome this lack of information, a transmittance model (TM) has been previously developed and enhanced by the authors to derive the atmospheric transmittance between a heliostat and receiver on the basis of common direct normal irradiance (DNI), temperature, relative humidity and barometric pressure measurements. Previously the model was only tested at one site. In this manuscript, the enhanced TM is validated for three sites (CIEMAT’s Plataforma Solar de Almería (PSA), Spain, Missour, Morocco (MIS) and Zagora, Morocco (ZAG)). As the strongest assumption in the TM is the vertical aerosol particle profile, three different approaches to describe the vertical profile are tested in the TM. One approach assumes a homogeneous aerosol profile up to 1 kilometer above ground, the second approach is based on LIVAS profiles obtained from Lidar measurements and the third approach uses boundary layer height (BLH) data of the European Centre for Medium-Range Weather Forecasts (ECMWF). The derived broadband transmittance for a slant range of 1 km (
【 授权许可】
Unknown