In this paper, a method previously developed for reconstructing daily erythemal ultraviolet (UV ery ) doses in Novi Sad (Serbia) was improved and used for estimating daily UV ery over the period 1971-2018. The proposed new method uses reanalysed total ozone column (TOC) data and snow cover as an input and is based on the empirical relationship between relative sunshine duration and relative UV ery doses. Introducing reanalysed TOC data and snow cover data significantly improved the quality and accuracy of the reconstructed UV ery time series, particularly in the winter season. The reconstructed time series revealed the statistically significant increase in summer and winter UV ery in the 1980s and the first half of the 1990s (+8.78% and + 13.14% per decade, respectively), which was linked to the statistically significant decline in TOC (−4.13 and −7.36% per decade, respectively). The study focuses on days with high erythemal UV dose ( high UV ery ), which is defined based on the 90th percentile of the daily UV ery for each month. Moreover, the influence of low TOC, low cloud cover conditions, and high surface albedo on high UV ery was analysed on a seasonal basis. The results of this study show that high UV ery days increased from the 1980s, particularly strongly in the period of TOC depletion. A fraction of high UV ery days in the last two decades was large (12.29%), which is higher than in the previous periods (6.97 and 8.68% in the period before and during TOC depletion, respectively). The occurrence of high UV ery days was influenced mostly by low cloud cover (89.71% of days), and low TOC (82.23% of days). In the winter season, high surface albedo influenced the appearance of 19.18% of high UV ery days. However, overall the interaction of low cloud cover and low TOC in all seasons most often led to the appearance of high UV ery days.