What we know about aerosol reduction
It will probably worsen heatwaves, especially in the northern hemisphere which is bad news if it penetrates into the arctic circle, like with last year’s Siberian and Canadian heatwave, or for arctic centred heatwaves like we had in northern Greenland
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019GL082269It can strengthen the jet stream in winter, when localized in eurasia, because of warming, lessening extreme weathers outside the arctic, so probably good news for the refreeze given that most aerosol is concentrated away from the arctic.
https://www.nature.com/articles/s41558-020-0693-4tThere is further evidence that aerosols could inhibit thermal contrast between land and sea, in east Asia, as well as further evidence that they reduce insolation
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2015RG000500In contrast of the decreased surface insolation, aerosols increase air Temperatures, which seems less important on melting ice, but they also are the cause of more stormy events as opposed to light rain, which will have a definite differentiated impact on the melting season, though I cannot guess which, and on the freezing season with probably earlier refreeze due to less storm events but lesser refreeze due to more ubiquitous snow cover. As the study concentrates on a blackspot for aerosols, it will probably be a much lesser impact in the arctic.
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2019JD030758Finally there is a feedback loop that increases aerosol concentration, stabilizing it in place, along with the atmosphere, with the creation of a heat gradient. It being broken could paradoxically mean more aerosols in the arctic for a little while (so opposite effects to those discussed above) and more chaos in an already volatile weather and climate system.
https://academic.oup.com/nsr/article/4/6/810/4191281Additionally another feedback loop between reduced precipitation and higher aerosol concentration, also tributary to the same atmospheric stabilization, strengthens the case for increased precipitations and chaos in the system with reduction in aerosol, although locally
https://opensky.ucar.edu/islandora/object/articles%3A7038/datastream/PDF/download/citation.pdfOverall, simulations tend to agree that its macro effect is additional melt within the arctic
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1002/2015GL065504?campaign=wlytk-41855.6211458333And, warming in various world regions
https://iopscience.iop.org/article/10.1088/1748-9326/ab6b34Additional links
https://eos.org/editors-vox/intensified-investigations-of-east-asian-aerosols-and-climatehttps://ftp.cpc.ncep.noaa.gov/hwang/Papers_pdf/Publication_2007-present/2008_Zhang_JGR.pdf (Could mean a change in moisture repartition in a reduction event if taken along with the feedback article)