The aerosol influence on the more recent transition
phase from dimming to brightening and the subsequent
brightening is better documented. Wild et al. [2005] examined
SSR at worldwide distributed BSRN stations and
found brightening tendencies during the 1990s not only
under all-sky conditions, but also in cloud-free conditions.
This indicates that aerosol changes may have contributed to
the recent brightening. Streets et al. [2006] noted a qualitative
agreement between changes in the anthropogenic
emissions of sulphur and black carbon and the widespread
transition from dimming to brightening found by Wild et al.
[2005] in various regions around the world. The historic
emission inventories suggest that global sulfur emissions
peaked in late 1980s, and decreased thereafter [Stern, 2006;
Streets et al., 2006]. The decline in the emissions of sulphur
and black carbon was particularly strong in large areas of
the industrialized world over the period 1980–2000, after
increases in previous decades [Streets et al., 2006], in line
with the changes noted in the SSR records. This reversal in
the emission trends is likely related, on one hand, to the air
pollution legislations that have started to become effective
in many developed nations in the 1980s. On the other
hand, economic crises also led to reduced emissions in
eastern Europe and the former Soviet Union from the late
1980s onward, and in Asia in the 1990s [Streets et al.,
2009].