Models
suggest atmospheric aerosol concentrations will increase as the temperatures keep climbing — and that's bad news for your lungs.
Not exact matches
Computer models
suggest that deploying
aerosols can have «an appreciable impact on tropical cyclone intensity,» writes William Cotton, an
atmospheric scientist at Colorado State University.
Basic physical science considerations, exploratory climate modeling, and the impacts of volcanic
aerosols on climate all
suggest that SWCE could partially compensate for some effects — particularly net global warming — of increased
atmospheric CO2.
Research published in 2008 by Arizona State University professor Peter Crozier
suggests that this nanoscale
atmospheric aerosol species is abundant in the atmosphere over East Asian countries and should be explicitly included in models of radiative forcing (the gap between energy radiation reaching the Earth and that leaving through the upper atmosphere).
The annual average is about 0.25 of the peak — but you expect as well that the reflected SW would not vary as much as you
suggest albedo of oceans being influenced by «solar zenith angle, wind speed, transmission by
atmospheric cloud /
aerosol, and ocean chlorophyll concentration.»
Both articles are based on peer reviewed published papers that
suggest volcanic
aerosols have played a part in the recent slow down of
atmospheric warming.
Recently it was
suggested that the formation of new
atmospheric aerosol particles is connected with the existence of thermodynamically stable 1 - to 2 - nm clusters, formed in the atmosphere by some nucleation mechanism.
Model calculations
suggest that almost half of the global cloud condensation nuclei in the
atmospheric boundary layer may originate from the nucleation of
aerosols from trace condensable vapours4, although the sensitivity of the number of cloud condensation nuclei to changes of nucleation rate may be small5, 6.
Feulner's work is a reanalysis of Weber (2010), which strongly
suggested that cosmic rays cause a large part of
atmospheric aerosol formation.