Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation
A generally accepted value for the Radiation Amplification Factor (RAF), with respect to the erythemal action spectrum for sunburn of human skin, is −1.1, indicating that a 1.0% increase in stratospheric ozone leads to a 1.1% decrease in the biologically damaging UV radiation in the erythemal action...
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MDPI AG
2017-08-01
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Online Access: | https://www.mdpi.com/2073-4433/8/8/153 |
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author | Eric S. Hall |
author_facet | Eric S. Hall |
author_sort | Eric S. Hall |
collection | DOAJ |
description | A generally accepted value for the Radiation Amplification Factor (RAF), with respect to the erythemal action spectrum for sunburn of human skin, is −1.1, indicating that a 1.0% increase in stratospheric ozone leads to a 1.1% decrease in the biologically damaging UV radiation in the erythemal action spectrum reaching the Earth. The RAF is used to quantify the non-linear change in the biologically damaging UV radiation in the erythemal action spectrum as a function of total column ozone (O3). Spectrophotometer measurements recorded at ten US monitoring sites were used in this analysis, and over 71,000 total UVR measurement scans of the sky were collected at those 10 sites between 1998 and 2000 to assess the RAF value. This UVR dataset was examined to determine the specific impact of clouds on the RAF. Five de novo modeling approaches were used on the dataset, and the calculated RAF values ranged from a low of −0.80 to a high of −1.38. |
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issn | 2073-4433 |
language | English |
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spelling | doaj.art-5f02d14addf34c2a8133258ad11eeb0f2022-12-21T18:26:30ZengMDPI AGAtmosphere2073-44332017-08-018815310.3390/atmos8080153atmos8080153Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet RadiationEric S. Hall0National Exposure Research Laboratory, Office of Research and Development, US Environmental Protection Agency, Mail Drop E205-03, 109 T. W. Alexander Drive, Research Triangle Park, NC 27711, USAA generally accepted value for the Radiation Amplification Factor (RAF), with respect to the erythemal action spectrum for sunburn of human skin, is −1.1, indicating that a 1.0% increase in stratospheric ozone leads to a 1.1% decrease in the biologically damaging UV radiation in the erythemal action spectrum reaching the Earth. The RAF is used to quantify the non-linear change in the biologically damaging UV radiation in the erythemal action spectrum as a function of total column ozone (O3). Spectrophotometer measurements recorded at ten US monitoring sites were used in this analysis, and over 71,000 total UVR measurement scans of the sky were collected at those 10 sites between 1998 and 2000 to assess the RAF value. This UVR dataset was examined to determine the specific impact of clouds on the RAF. Five de novo modeling approaches were used on the dataset, and the calculated RAF values ranged from a low of −0.80 to a high of −1.38.https://www.mdpi.com/2073-4433/8/8/153Radiation Amplification Factor (RAF)solar zenith angle (SZA)Dobson Unit (DU)ultraviolet (UV)ultraviolet radiation (UVR)cloudiness |
spellingShingle | Eric S. Hall Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation Atmosphere Radiation Amplification Factor (RAF) solar zenith angle (SZA) Dobson Unit (DU) ultraviolet (UV) ultraviolet radiation (UVR) cloudiness |
title | Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation |
title_full | Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation |
title_fullStr | Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation |
title_full_unstemmed | Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation |
title_short | Comparison of Five Modeling Approaches to Quantify and Estimate the Effect of Clouds on the Radiation Amplification Factor (RAF) for Solar Ultraviolet Radiation |
title_sort | comparison of five modeling approaches to quantify and estimate the effect of clouds on the radiation amplification factor raf for solar ultraviolet radiation |
topic | Radiation Amplification Factor (RAF) solar zenith angle (SZA) Dobson Unit (DU) ultraviolet (UV) ultraviolet radiation (UVR) cloudiness |
url | https://www.mdpi.com/2073-4433/8/8/153 |
work_keys_str_mv | AT ericshall comparisonoffivemodelingapproachestoquantifyandestimatetheeffectofcloudsontheradiationamplificationfactorrafforsolarultravioletradiation |