Not exact matches
Analyses of the ground and aircraft data performed by Setyan et al. (2012), Shilling et al. (2013), and Kleinman et al. (2016) showed that organic
aerosol production increased when human - caused emissions from Sacramento mixed
with air rich in isoprene, an organic compound wafting from many plants that originate in the area's foothills.
To go farther, though, and count on offsetting the entire unrestrained CO2
production of the coming century
with engineered
aerosols is fraught
with peril.
I write it off as a very real effect that is not well characterized by the models, probably because these models don't model
with enough accuracy the effect of the additional
aerosol particles on cloud
production to properly account for it's full effect on temperature.
Fertilizer
production will almost certainly keep growing to keep pace
with human population, but the amount of
aerosols created as a result depends on many factors, including air temperature, precipitation, season, time of day, wind patterns and of course the other needed ingredients from industrial or natural sources.
Associated
with human greenhouse gas
production is the release of fine particle known as
aerosols which have a temporary cooling effect (they last in the atmosphere less than a week).
The response of biogenic secondary organic carbon
aerosol production to a temperature change, however, could be considerably lower than the response of biogenic VOC emissions since
aerosol yields can decrease
with increasing temperature.
A growing number of studies perform both the chemical
production, transformation, and transportation of
aerosols and the radiative forcing calculations (see Chapter 5)
with the advantage of correlating predicted
aerosol distributions precisely
with fields determining
aerosol production and deposition such as clouds (e.g., Penner et al., 1998b).
Anthropogenic tropospheric
aerosol production trends correlating
with temperature trends.