«
On the other hand, we might assume that there has been some lower, but non-zero «background level» of volcanic aerosols - let's arbitrarily make it 2 on a scale of 10, for ease of discussio
On the other hand, we might assume that there has been some lower, but non-zero «
background level» of volcanic
aerosols - let's arbitrarily make it 2
on a scale of 10, for ease of discussio
on a scale of 10, for ease of discussion.
Together with potentially increased tropical
aerosol concentrations, they might even have an impact
on the stratospheric
background AOD currently (Vernier et al..
These clouds then glaciate in higher levels, which could result in either more or less vigorous precipitation formation depending
on the
background aerosol levels and atmospheric stability (Khain et al., 2004).