Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies
Solar blue-violet wavelengths (380−455 nm) are at the high energy end of the visible spectrum; referred to as “high energy visible” (<i>HEV</i>). Both chronic and acute exposure to these wavelengths has been often highlighted as a cause for concern with respect to ocular health. The sun...
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| Format: | Article |
| Language: | English |
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MDPI AG
2020-07-01
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| Series: | Sensors |
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| Online Access: | https://www.mdpi.com/1424-8220/20/15/4105 |
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| author | Alfio V. Parisi Damien P. Igoe Abdurazaq Amar Nathan J. Downs |
| author_facet | Alfio V. Parisi Damien P. Igoe Abdurazaq Amar Nathan J. Downs |
| author_sort | Alfio V. Parisi |
| collection | DOAJ |
| description | Solar blue-violet wavelengths (380−455 nm) are at the high energy end of the visible spectrum; referred to as “high energy visible” (<i>HEV</i>). Both chronic and acute exposure to these wavelengths has been often highlighted as a cause for concern with respect to ocular health. The sun is the source of <i>HEV</i> which reaches the Earth’s surface either directly or after scattering by the atmosphere and clouds. This research has investigated the effect of clouds on <i>HEV</i> for low solar elevation (solar zenith angles between 60° and 80°), simulating time periods when the opportunity for ocular exposure in global populations with office jobs is high during the early morning and late afternoon. The enhancement of “bluing” of the sky due to the influence of clouds was found to increase significantly with the amount of cloud. A method is presented for calculating <i>HEV</i> irradiance at sub-tropical latitudes from the more commonly measured global solar radiation (300–3000 nm) for all cases when clouds do and do not obscure the sun. The method; when applied to global solar radiation data correlates well with measured <i>HEV</i> within the solar zenith angle range 60° and 80° (R<sup>2</sup> = 0.82; mean bias error (MBE) = −1.62%, mean absolute bias error (MABE) = 10.3% and root mean square error (RMSE) = 14.6%). The technique can be used to develop repeatable <i>HEV</i> hazard evaluations for human ocular health applications |
| first_indexed | 2024-03-10T18:16:07Z |
| format | Article |
| id | doaj.art-9a5cff88f8ee45bdb2c5c8592aa17d4d |
| institution | Directory Open Access Journal |
| issn | 1424-8220 |
| language | English |
| last_indexed | 2024-03-10T18:16:07Z |
| publishDate | 2020-07-01 |
| publisher | MDPI AG |
| record_format | Article |
| series | Sensors |
| spelling | doaj.art-9a5cff88f8ee45bdb2c5c8592aa17d4d2023-11-20T07:42:53ZengMDPI AGSensors1424-82202020-07-012015410510.3390/s20154105Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected SkiesAlfio V. Parisi0Damien P. Igoe1Abdurazaq Amar2Nathan J. Downs3Faculty of Health, Engineering and Sciences, University of Southern Queensland, Toowoomba 4350, AustraliaFaculty of Health, Engineering and Sciences, University of Southern Queensland, Toowoomba 4350, AustraliaFaculty of Health, Engineering and Sciences, University of Southern Queensland, Toowoomba 4350, AustraliaFaculty of Health, Engineering and Sciences, University of Southern Queensland, Toowoomba 4350, AustraliaSolar blue-violet wavelengths (380−455 nm) are at the high energy end of the visible spectrum; referred to as “high energy visible” (<i>HEV</i>). Both chronic and acute exposure to these wavelengths has been often highlighted as a cause for concern with respect to ocular health. The sun is the source of <i>HEV</i> which reaches the Earth’s surface either directly or after scattering by the atmosphere and clouds. This research has investigated the effect of clouds on <i>HEV</i> for low solar elevation (solar zenith angles between 60° and 80°), simulating time periods when the opportunity for ocular exposure in global populations with office jobs is high during the early morning and late afternoon. The enhancement of “bluing” of the sky due to the influence of clouds was found to increase significantly with the amount of cloud. A method is presented for calculating <i>HEV</i> irradiance at sub-tropical latitudes from the more commonly measured global solar radiation (300–3000 nm) for all cases when clouds do and do not obscure the sun. The method; when applied to global solar radiation data correlates well with measured <i>HEV</i> within the solar zenith angle range 60° and 80° (R<sup>2</sup> = 0.82; mean bias error (MBE) = −1.62%, mean absolute bias error (MABE) = 10.3% and root mean square error (RMSE) = 14.6%). The technique can be used to develop repeatable <i>HEV</i> hazard evaluations for human ocular health applicationshttps://www.mdpi.com/1424-8220/20/15/4105cloud modification factorvisible radiationinstrumentationhigh energy visibleblue light |
| spellingShingle | Alfio V. Parisi Damien P. Igoe Abdurazaq Amar Nathan J. Downs Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies Sensors cloud modification factor visible radiation instrumentation high energy visible blue light |
| title | Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies |
| title_full | Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies |
| title_fullStr | Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies |
| title_full_unstemmed | Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies |
| title_short | Solar Blue Light Radiation Enhancement during Mid to Low Solar Elevation Periods under Cloud Affected Skies |
| title_sort | solar blue light radiation enhancement during mid to low solar elevation periods under cloud affected skies |
| topic | cloud modification factor visible radiation instrumentation high energy visible blue light |
| url | https://www.mdpi.com/1424-8220/20/15/4105 |
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