Figure 1 shows increasing trend (confidence level: 99%) of annual accumulation of daily erythemal UV radiation at Tsukuba during the overall observation period, with an increase rate of 4.6% per decade (33.0 kJ/m2 per decade). As per "Long-term Trends of Total Ozone," total ozone shows a slight increase in the 1990s and early 2000s, with no discernible trend in recent years. Accordingly, the increasing trend in erythemal UV radiation cannot be explained solely by overall ozone changes. This may be attributed to a decreasing tendency in aerosol optical extinction, air pollution and/or the weather condition changes over monitoring sites such as cloudiness (UNEP, 2022).
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UNEP (2022), Environmental effects of stratospheric ozone depletion, UV radiation, and interactions with climate change: 2022 assessment report.