2005
DOI: 10.3846/16486897.2005.9636843
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Ultraviolet Radiation and Ground‐level Ozone Variation in Lithuania

Abstract: Preliminary analysis of the data of ultraviolet (UV) radiation and ground‐level ozone concentration measurements from Rugšteliškes Monitoring Station over the years 2002–2003 is presented. Observations showed that an average UV radiation value in January and July of 2002 differed about 10 times. Maximum intensity of UVA radiation was observed in July (about 2,4 W/m2), and minimal one ‐ in December (0,1 W/m2), the highest UVB radiation intensity was in May (0,09 W/m2), while a minimal UVB radiation value as wel… Show more

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Cited by 11 publications
(9 citation statements)
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“…In the ambient atmosphere, a portion of the UV light in the spectral region of 290–400 nm can reach the Earth’s surface, while UV light with wavelengths below 290 nm (used here to generate OH from O 3 ) is completely absorbed by the O 3 layer . Hence, to more realistically simulate the atmosphere, OH initiated photo-oxidation experiments were also performed using 302 nm UV lamp irradiation which is both present in the atmosphere and able to activate TiO 2 .…”
Section: Resultsmentioning
confidence: 99%
See 1 more Smart Citation
“…In the ambient atmosphere, a portion of the UV light in the spectral region of 290–400 nm can reach the Earth’s surface, while UV light with wavelengths below 290 nm (used here to generate OH from O 3 ) is completely absorbed by the O 3 layer . Hence, to more realistically simulate the atmosphere, OH initiated photo-oxidation experiments were also performed using 302 nm UV lamp irradiation which is both present in the atmosphere and able to activate TiO 2 .…”
Section: Resultsmentioning
confidence: 99%
“…In the ambient atmosphere, a portion of the UV light in the spectral region of 290−400 nm can reach the Earth's surface, while UV light with wavelengths below 290 nm (used here to generate OH from O 3 ) is completely absorbed by the O 3 layer. 52 Hence, to more realistically simulate the atmosphere, OH initiated photo-oxidation experiments were also performed using 302 nm UV lamp irradiation which is both present in the atmosphere and able to activate TiO 2 . 18 As expected, 53 due to the lower photochemical activity of TiO 2 at 302 nm UV light irradiation (vs 254 nm), the measured O/C of SOM Ti (302 nm) across all photochemical ages is lower than that of SOM Ti (254 nm) but higher than that of SOM Si (254 nm), as shown in Figure 2B.…”
Section: ■ Results and Discussionmentioning
confidence: 99%
“…Seasonally, the highest intensity of UV ray is measured during spring and summer whereas the minimal presence of UV radiation is registered during winter. The wavelength of UV ray which invades to the surface of the earth is varied within 290 nm to 400 nm (Chadyšiene et al 2005 ). The entire UV-A radiation reaches to the earth’s surface as there is no incident of UV-A absorption by atmospheric ozone (Tan et al 2018 ) while UV-C is wholly engrossed by ozone and oxygen in the upper and middle portion of the atmosphere (Chandra and Mcpeters 1994 ).…”
Section: Discussionmentioning
confidence: 99%
“…including snow, sand, and water have much higher UV intensity than in other areas, and the reflectivity of these surfaces toward UVA and UVB is different. [137] Without taking all these factors into account, the sensor algorithm may introduce some errors during estimation of the UVB exposure.…”
Section: Wwwadvmattechnoldementioning
confidence: 99%