• Slavica Malinović-Milićević University of Novi Sad, ACIMSI — University Center for Meteorology and Environmental Modelling, Novi Sad
  • Zoran Mijatović University of Novi Sad, Faculty of Sciences, Department of Physics, Novi Sad
  • Ilija Arsenić University of Novi Sad, Faculty of Agriculture, Novi Sad
  • Zorica Podrašćanin University of Novi Sad, Faculty of Sciences, Department of Physics, Novi Sad
  • Ana Firanj Sremac University of Novi Sad, Faculty of Agriculture, Novi Sad
  • Milan Radovanović Geographical Institute “Jovan Cvijić” SASA, Belgrade; South Ural State University, Institute of Sports, Tourism and Service, Chelyabinsk
  • Nusret Drešković University of Sarajevo, Faculty of Sciences, Department of Geography, Sarajevo



UV radiation, ozone, measurements, estimation


Solar ultraviolet (UV) radiation is a significant health hazard in the warm part of the year. In order to assess the level of hazard and the effects of UV radiation on the living world, long-term measured or estimated data are needed. In Novi Sad, the measurement of UV radiation has been performed since 2003, while ozone measurements have been made since 2007. However, those data sets are too short for assessing long-term biological effects. Therefore, several techniques for reconstruction of UV radiation doses have been developed. Reconstruction techniques are based on using available ground-based measurements of the meteorological data and satellite measurements of the total ozone column. It is shown that techniques that use ozone data show better performance than those that use only ground-based meteorological measurements. However, the difference between the performances of the methods is smaller when it comes to the monthly values, indicating that the techniques which use only ground-based meteorological measurements are roughly as good as the ozone-based techniques for assessing long-term changes in the surface UV radiation. The statistically significant increasing long term-trend of annual mean erythemal UV doses (ERY) and the decreasing trend in the total ozone column in Novi Sad since 1981 have been noticed. An increase in ERY has been noticed in all the seasons except in autumn and it is the highest in winter. The analysis showed that the increase in the ERY in the period 1981–1996 was mainly caused by the total ozone column, while the increase after 1996 is largely caused by cloudiness.

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Anton, M., Serrano, A., Cancillo, M. L., & Garcia, J. A. (2008). Relationship between erythemal irradiance and total solar irradiance in South Western Spain. Journal of Geophysical Research: Atmospheres, 113, D14208.

Dichter, B. K., Beaubien, A. F., & Beaubien, D. J. (1993). Development and characterization of a new solar ultraviolet-B irradiance detector. Journal of Atmospheric and Oceanic Technology, 10(3), 337–344.<0337:DACOAN>2.0.CO;2

Gallagher, R. P., & Lee, T. K. (2006). Adverse effects of ultraviolet radiation: a brief review. Progress in Biophysics and Molecular Biology, 92(1), 119–131.

Jégou, F., Godin-Beekman, G., Corrêa. M. P., Brogniez, C., Auriol, F., Peuch, V. H., . . . Mahé, E. (2011). Validity of satellite measurements used for the monitoring of UV radiation risk on health. Atmospheric Chemistry and Physics, 11, 13377–13394.

Levelt, P. F., van den Oord, G. H., Dobber, M. R., Malkki, A., Visser, H., de Vries, J., . . . Saari, H. (2006). The ozone monitoring instrument. IEEE Transactions on geoscience and remote sensing, 44(5), 1093–1101.

Lindfors, A., & Vuilleumier, L. (2005). Erythemal UVat Davos (Switzerland), 1926–2003, estimated using total ozone, sunshine duration, and snow depth. Journal of Geophysical Research: Atmospheres, 110, D02104.

Malinović, S. (2003). A model for the prognosis of the intensity of UV radiation using the numerical weather prediction model (Unpublished master's thesis). University of Novi Sad, Novi Sad, Serbia.

Malinovic, S., Mihailovic, D. T., Kapor, D., Mijatovic, Z., & Arsenic, I. D. (2006). NEOPLANTA: a short description of the first Serbian UV index model. Journal of Applied Meteorology and Climatology, 45(8), 1171–1177.

Malinović-Milićević, S. (2012). Monitoring of the non-ionizing radiation, air pollution and heat indexes in Vojvodina region (Unpublished doctoral dissertation). University of Novi Sad, Novi Sad, Serbia.

Malinovic-Milicevic, S., & Mihailovic, D. T. (2011). The use of NEOPLANTA model for evaluating the UV index in the Vojvodina region (Serbia). Atmospheric Research, 101(3), 621–630.

Malinovic-Milicevic, S., Mihailovic, D. T., Drešković, N., Đurđević, V., Mimić, G., & Arsenić, I. (2015). Climate Change effects and UV-B radiation in the Vojvodina region (Serbia) under the SRES-A2. Thermal Science, 19(2), S289–S298.

Malinovic-Milicevic, S., Mihailovic, D. T., Lalic, B., & Dreskovic, N. (2013). Thermal environment and UV-B radiation indices in the Vojvodina region (Serbia). Climate Research, 57(2), 111–121.

Malinovic-Milicevic, S., Mihailovic, D. T., & Radovanovic, M. M. (2015). Reconstruction of the erythemal UV radiation data in Novi Sad (Serbia) using the NEOPLANTA parametric model. Theoretical and Applied Climatology, 121(1–2), 131–138.

Malinovic-Milicevic, S., Vyklyuk, Y., Radovanovic, M. M., & Petrovic, M. D. (2018). Long-term erythemal ultraviolet radiation in Novi Sad (Serbia) reconstructed by neural network modeling. International Journal of Climatology, 38(8), 3264–3272.

Mateos Villán, D., de Miguel Castrillo, A., & Bilbao Santos, J. (2010). Empirical models of UV total radiation and cloud effect study. International Journal of Climatology, 30(9), 1407–1415.

McKinley, A. F., & Diffey, B. L. (1987). A reference action spectrum for ultraviolet induced erythema in human skin. CIE-Journal, 6, 17–22.

Mijatović, Z., Milićević, S., Kapor, D., Mihailović, D., Arsenić, I., & Podrašćanin, Z. (2010). Solar UV radiation: monitoring and new approach in modelling - pioneering work in Serbia. In D. T. Mihailović & B. Lalić (Eds.), Advances in environmental modeling and measurements (pp. 113–119). New York, NY: Nova Science.

Morys, M., Mims III, F. M., Hagerup, S., Anderson, S. E., Baker, A., Kia, J., & Walkup, T. (2001). Design, calibration, and performance of MICROTOPS II handheld ozone monitor and Sun photometer. Journal of Geophysical Research: Atmospheres, 106(D13), 14573–14582.

NASA. (2010) Total Ozone Mapping Spectroradiometer. Retrieved December 15, 2010, from

NASA Goddard Earth Sciences Data and Information Services Center. (2017). Giovanni: The Bridge Between Data and Science (version 4.22) [Web application]. Retrieved from

Podrascanin, Z., Balog, I., Jankovic, A., Mijatovic, Z., & Nadj, Z. (2017). A Comparison of MICROTOPS II and OMI Satellite Ozone Measurements in Novi Sad from 2007 to 2015. Pure and Applied Geophysics, 174(12), 4489–4499.

Reuder, J., & Koepke, P. (2005). Reconstruction of UV radiation over Southern Germany for the past decades. Meteorologische Zeitschrift, 14(2), 237–246.

Rieder, H. E., Holawe, F., Simic, S., Blumthaler, M., Krzyścin, J. W., Wagner, J. E., . . . Weihs, P. (2008). Reconstruction of erythemal UV-doses for two stations in Austria: A comparison between alpine and urban regions. Atmospheric Chemistry and Physics, 8(20), 6309–6323.

Schmalwieser, A. W., Gröbner, J., Blumthaler, M., Klotz, B., De Backer, H., Bolsée, D., . . . O'Hagan, J. (2017). UV Index monitoring in Europe. Photochemical & Photobiological Sciences, 16(9), 1349–1370.

UV index. (n.d.).

Vanicek, K., Frei, T., Litynska, Z., & Schmalwieser, A. (2000). UV-Index for the Public. A guide for publication and interpretation of solar UV Index forecasts for the public Working Group 4 of the COST-713 Action “UVB Forecasting". COST-713 Action. Luxembourg: Office for Official Publications of the European Communities.

Veefkind, J. P., de Haan, J. F., Brinksma, E. J., Kroon, M., & Levelt, P. F. (2006). Total ozone from the Ozone Monitoring Instrument (OMI) using the DOAS technique. IEEE Transactions on Geoscience and Remote Sensing, 44(5), 1239–1244.

Webb, A. R. (2000). Ozone Depletion and Changes in Environmental UV-B Radiation. In R. E. Hester & R. M. Harrison (Eds.), Causes and Environmental Implications of Increased UV-B Radiation (pp. 17–36).

World Health Organization. (1995). Protection against exposure to ultraviolet radiation (Tech. Rep. WHO/EHG 17). Retrieved from

World Health Organization. (2002). Global Solar UV Index: A Practical Guide. Retrieved from

World Meteorological Organization. (1997). Report of the WMO–WHO meeting of experts on standardization of UV Indices and their dissemination to the public (WMO/TD-No. 921). Retrieved from

Word Meteorological Organization. (1998). Guidelines for Site Quality Control of UV Monitoring (WMO/TD-No. 884, GAW Report- No. 126). Retrieved from

Word Meteorological Organization. (2008). Instruments to measure solar ultraviolet radiation - Part 2, Broadband Instruments Measuring Erythemally Weighted Solar Irradiance (WMO/TD- No. 1289; GAW Report- No. 164). Retrieved from




How to Cite

Malinović-Milićević, S., Mijatović, Z., Arsenić, I., Podrašćanin, Z., Firanj Sremac, A., Radovanović, M., & Drešković, N. (2020). THE IMPORTANCE OF GROUND-BASED AND SATELLITE OBSERVATIONS FOR MONITORING AND ESTIMATION OF UV RADIATION IN NOVI SAD (SERBIA). Journal of the Geographical Institute “Jovan Cvijić” SASA, 70(1), 57–70.

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