DOI: 10.1016/j.atmosenv.2014.10.005
Scopus记录号: 2-s2.0-84908402033
论文题名: Total ozone column, water vapour and aerosol effects on erythemal and global solar irradiance in Marsaxlokk, Malta
作者: Bilbao J ; , Román R ; , Yousif C ; , Mateos D ; , de Miguel A
刊名: Atmospheric Environment
ISSN: 0168-2563
EISSN: 1573-515X
出版年: 2014
卷: 99 起始页码: 508
结束页码: 518
语种: 英语
英文关键词: Aerosol
; Central mediterranean
; Erythemal ultraviolet irradiance
; Total ozone column
; Total solar shortwave irradiance
; Water vapour column
Scopus关键词: Central Mediterranean
; Total ozone column
; Total solar shortwave irradiance
; Ultraviolet irradiance
; Water vapour
; Aerosols
; ozone
; aerosol
; Article
; atmosphere
; attenuation
; light irradiance
; Malta
; measurement
; optical depth
; radiation
; solar radiation
; ultraviolet radiation
; water vapor
Scopus学科分类: Environmental Science: Water Science and Technology
; Earth and Planetary Sciences: Earth-Surface Processes
; Environmental Science: Environmental Chemistry
英文摘要: Observations of erythemal (UVER; 280-400nm) and total solar shortwave irradiance (SW; 305-2800nm), total ozone column (TOC), water vapour column (w), aerosol optical depth (AOD) and Ångström exponent (α) were carried out at Marsaxlokk, in south-east Malta. These measurements were recorded during a measurement campaign between May and October 2012, aimed at studying the influence of atmospheric compounds on solar radiation transfer through the atmosphere. The effects of TOC, AOD and w on UVER and SW (global, diffuse and direct) irradiance were quantified using irradiance values under cloud-free conditions at different fixed solar zenith angles (SZA). Results show that UVER (but not SW) irradiance correlates well with TOC. UVER variations ranged between-0.24%DU-1 and-0.32%DU-1 with all changes being statistically significant. Global SW irradiance varies with water vapour column between-2.44%cm-1 and-4.53%cm-1, these results proving statistically significant and diminishing when SZA increases. The irradiance variations range between 42.15%cm-1 and 20.30%cm-1 for diffuse SW when SZA varies between 20° and 70°. The effect of aerosols on global UVER is stronger than on global SW. Aerosols cause a UVER reduction of between 28.12% and 52.41% and a global SW reduction between 13.46% and 41.41% per AOD550 unit. Empirical results show that solar position plays a determinant role, that there is a negligible effect of ozone on SW radiation, and stronger attenuation by aerosol particles in UVER radiation. © 2014 Elsevier Ltd.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/80560
Appears in Collections: 气候变化事实与影响
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作者单位: Valladolid University, Laboratory of Atmosphere and Energy, Faculty of Sciences, Valladolid, Spain; University of Malta, Institute for Sustainable Energy, Marsaxlokk, Malta
Recommended Citation:
Bilbao J,, Román R,, Yousif C,et al. Total ozone column, water vapour and aerosol effects on erythemal and global solar irradiance in Marsaxlokk, Malta[J]. Atmospheric Environment,2014-01-01,99