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. Author manuscript; available in PMC: 2021 May 20.
Published in final edited form as: Photochem Photobiol Sci. 2020 May 20;19(5):542–584. doi: 10.1039/d0pp90011g

Table 1.

Comparison of zonal mean changes in clear-sky UVI calculated by Lamy et al.3 and Bais et al.1

Latitudes Lamy et al.3 Bais et al.1
Change [%] 1960 to 2100a Change [%] 2015 to 2090b Change [%] 2015 to 2090c
Transient AODs, RCP = Fixed AODs Transient AODs Fixed AODs Fixed AODs
2.6 4.5 6.0 8.5 RCP 6.0 RCP 6.0 RCP 6.0 RCP 6.0
Annual meane Jan Apr Jul Oct
High Nd 6 2 1 −8 −5 0 −6 −3 −7 −5 −4
30–60° N 8 5 5 −1 −2 5 −3 −4 −5 −3 −2
0–30° N 3 3 3 1 3 1 −1 0 −1 −1
0–30° S 3 3 3 2 3 0 0 −1 0 −1 −1
30–60° S 3 3 2 −2 0 −5 −6 −5 −4 −5 −6
High Sd 7 6 4 0 −2 −18 −18 −8 −6 −6 −23

All values are rounded. a According to Table 5 of Lamy et al.3 b Inferred from Fig. 4 and Fig. 6 of Lamy et al.3 c Table 1 of Bais et al.1 d Latitude range of “High northern (N)” and “High southern (S)” refer to 60–90° in Lamy et al.3 and 60–80° in Bais et al.1 e Trends reported by Lamy et al.3 refer to trends averaged over all months; Bais et al.1 provide trends for the months of January, April, July and October.