Surface Level Solar Ultraviolet-B Radiation At Penang

Broadband photometric measurements of solar UV-B, UV -A, global and diffuse radiation were made at Universiti Sains Malaysia (USM), Penang from 1994 to 2001. Results from this study show that the large temporal variations for the measured solar radiation is due to the dominant effect of solar zen...

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Main Author: Karuppusamy, Arunasala Pandy Ail
Format: Thesis
Language:English
Published: 2006
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Online Access:http://eprints.usm.my/55454/1/00001651776.pdf
http://eprints.usm.my/55454/
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spelling my.usm.eprints.55454 http://eprints.usm.my/55454/ Surface Level Solar Ultraviolet-B Radiation At Penang Karuppusamy, Arunasala Pandy Ail QC1 Physics (General) Broadband photometric measurements of solar UV-B, UV -A, global and diffuse radiation were made at Universiti Sains Malaysia (USM), Penang from 1994 to 2001. Results from this study show that the large temporal variations for the measured solar radiation is due to the dominant effect of solar zenith angle and clouds. Under all sky conditions, the mean daily total radiation values for the UV-B, UV-A and global radiation were 1.514 x 104 J m-2, 4.69 x lOS J m-2 and 1.80 x 107 J m-2 respectively. For cloudless sky days, the daily maximum UV-B and global irradiance were 1.372 W m-2 and 1.423 kW m-2. The measured effective UV-B irradiance was converted to the erythemal UV flux to relate it to the potential harmful effects due to UV exposure; UVB flux level is in the High or Extreme ranges between 1030 and 1530 hours local time. A study of the diurnal variation of the solar UV -B, UV-A and global radiation show that for similar zenith angles, the solar irradiance after solar noon is larger than that before solar noon. This assymmetrical effect is attributed to the scattering of solar radiation by clouds. Seasonal variation studies show a constant periodicity for the solar UV-B, UV-A and global flux with maximums in March and September. Using available meteorological parameters and total column ozone data, their effects on the surface level solar UV -B radiation was investigated. A mathematical model to estimate the surface level solar UV-8 radiation was also developed and compared with two established model. The spectral model performance is good with a mean error of9.9%. To compliment the spectral model, a simple empirical model was also formulated using multivariate analysis. The mean error of the empirical model was 2.5%. 2006-06 Thesis NonPeerReviewed application/pdf en http://eprints.usm.my/55454/1/00001651776.pdf Karuppusamy, Arunasala Pandy Ail (2006) Surface Level Solar Ultraviolet-B Radiation At Penang. PhD thesis, Perpustakaan Hamzah Sendut.
institution Universiti Sains Malaysia
building Hamzah Sendut Library
collection Institutional Repository
continent Asia
country Malaysia
content_provider Universiti Sains Malaysia
content_source USM Institutional Repository
url_provider http://eprints.usm.my/
language English
topic QC1 Physics (General)
spellingShingle QC1 Physics (General)
Karuppusamy, Arunasala Pandy Ail
Surface Level Solar Ultraviolet-B Radiation At Penang
description Broadband photometric measurements of solar UV-B, UV -A, global and diffuse radiation were made at Universiti Sains Malaysia (USM), Penang from 1994 to 2001. Results from this study show that the large temporal variations for the measured solar radiation is due to the dominant effect of solar zenith angle and clouds. Under all sky conditions, the mean daily total radiation values for the UV-B, UV-A and global radiation were 1.514 x 104 J m-2, 4.69 x lOS J m-2 and 1.80 x 107 J m-2 respectively. For cloudless sky days, the daily maximum UV-B and global irradiance were 1.372 W m-2 and 1.423 kW m-2. The measured effective UV-B irradiance was converted to the erythemal UV flux to relate it to the potential harmful effects due to UV exposure; UVB flux level is in the High or Extreme ranges between 1030 and 1530 hours local time. A study of the diurnal variation of the solar UV -B, UV-A and global radiation show that for similar zenith angles, the solar irradiance after solar noon is larger than that before solar noon. This assymmetrical effect is attributed to the scattering of solar radiation by clouds. Seasonal variation studies show a constant periodicity for the solar UV-B, UV-A and global flux with maximums in March and September. Using available meteorological parameters and total column ozone data, their effects on the surface level solar UV -B radiation was investigated. A mathematical model to estimate the surface level solar UV-8 radiation was also developed and compared with two established model. The spectral model performance is good with a mean error of9.9%. To compliment the spectral model, a simple empirical model was also formulated using multivariate analysis. The mean error of the empirical model was 2.5%.
format Thesis
author Karuppusamy, Arunasala Pandy Ail
author_facet Karuppusamy, Arunasala Pandy Ail
author_sort Karuppusamy, Arunasala Pandy Ail
title Surface Level Solar Ultraviolet-B Radiation At Penang
title_short Surface Level Solar Ultraviolet-B Radiation At Penang
title_full Surface Level Solar Ultraviolet-B Radiation At Penang
title_fullStr Surface Level Solar Ultraviolet-B Radiation At Penang
title_full_unstemmed Surface Level Solar Ultraviolet-B Radiation At Penang
title_sort surface level solar ultraviolet-b radiation at penang
publishDate 2006
url http://eprints.usm.my/55454/1/00001651776.pdf
http://eprints.usm.my/55454/
_version_ 1748703963518074880
score 13.211869