The use of NEOPLANTA model for evaluating the UV index in the Vojvodina region (Serbia)
The increase in ultraviolet (UV) radiation in the last several decades caused intensive activities in its monitoring and forecast all over the world. Due to lack of ground measurements of UV index (UVI) in the Vojvodina region (Serbia), the numerical methods are an alternative to estimate its value....
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Veröffentlicht in: | Atmospheric research 2011-08, Vol.101 (3), p.621-630 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | The increase in ultraviolet (UV) radiation in the last several decades caused intensive activities in its monitoring and forecast all over the world. Due to lack of ground measurements of UV index (UVI) in the Vojvodina region (Serbia), the numerical methods are an alternative to estimate its value. The values of the UVI in one hour time resolutions are calculated using the NEOPLANTA model. Model outputs have been compared with measurements recorded, during the spring and summer period of 2006, with the Yankee UVB-1 biometer located at the campus of the University of Novi Sad, Novi Sad (Serbia). Obtained results show a good agreement with the UVI values for low cloudiness, while the largest uncertainties are associated with the higher amounts of ones. The strong correlation (0.815) and small absolute value of the difference of standard deviations in the simulations and the observations (0.102) for data with cloudiness
≤
6 and UVI
≥
3 indicates good model performances. Based on the overall results it can be concluded, in an acceptable level of accuracy, that the outputs of the NEOPLANTA model are an acceptable data source in the monitoring program of the UV radiation in the Vojvodina region in places having no actual measurements.
► The usability of the NEOPLANTA model in the UVI monitoring program is considered. ► The NEOPLANTA model is described shortly including its main features. ► The model outputs were compared with measurements for different range of cloudiness. ► Correlation coefficient is over 0.8 when cloudiness is less than 6 tenths. ► The model outputs can be used for the spatial representation of UVI maximum values. |
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ISSN: | 0169-8095 1873-2895 |
DOI: | 10.1016/j.atmosres.2011.04.008 |