Articles | Volume 18, issue 10
https://doi.org/10.5194/acp-18-7739-2018
https://doi.org/10.5194/acp-18-7739-2018
Research article
 | 
01 Jun 2018
Research article |  | 01 Jun 2018

Comparison of the optical depth of total ozone and atmospheric aerosols in Poprad-Gánovce, Slovakia

Peter Hrabčák

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Cited articles

Alpert, P., Shvainshtein, O., and Kishcha, P.: AOD trends over megacities based on space monitoring using MODIS and MISR, Am. J. Clim. Change, 12, 117–131, https://doi.org/10.4236/ajcc.2012.13010, 2012.
Arola, A. and Koskela, T.: On the sources of bias in aerosol optical depth retrieval in the UV range, J. Geophys. Res., 109, D08209, https://doi.org/10.1029/2003JD004375, 2004.
Bass, A. M. and Paur, R. J.: The ultraviolet cross-sections of ozone. I. The measurements, II. Results and temperature dependence, in: Atmospheric ozone, Proceedings of the Quadrennial ozone symposium, 3–7 September 1984, Halkidiki, Greece, 606–616, 1985.
Bodhaine, B. A., Wood, N. B., Dutton, E. G., and Slusser, J. R.: On Rayleigh Optical Depth Calculations, J. Atmos. Ocean. Tech., 16, 1854–1861, 1999.
Brewer, A.: A replacement for the Dobson spectrophotometer?, Pure Appl. Geophys., 106, 919–927, 1973.
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The paper presents results of a Brewer MKIV optical depth measurements from 1994 to 2016. The optical depth values were determined for the wavelengths of 306.3, 310, 313.5, 316.8 and 320 nm. The Langley plot method was applied to calculate the aerosols optical depth. A statistically significant decrease in the total optical depth of the atmosphere was observed with all examined wavelengths. Its root cause is the statistically significant decline in the optical depth of aerosols.
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