In the year with strong wave energy, by contrast, the lower stratospheric
warming in July and August leads to reduced ozone losses
throughout the Southern Hemisphere spring, when the
sunlight that powers ozone depletion chemistry returns to the polar regions.
Even in the absence of such an index, I believe it's well established that tree / plant area has increased in the last 30 years or so, in which case land use forcing (or at least the albedo part) would have been getting less negative for the period, adding to the
warming trend; and that's without counting asphalt which obviously has greater
sunlight absorption than the average land it replaces (and asphalt - covered surface has kept growing
throughout this period).