«Geoengineering» by reducing insolation
with aerosols in the stratosphere will also reduce the effectiveness of solar panels.
Not exact matches
OMPS is a three - part instrument: a nadir mapper that maps ozone, SO2 and
aerosols; a nadir profiler that measures the vertical distribution of ozone
in the
stratosphere; and a limb profiler that measures
aerosols in the upper troposphere,
stratosphere and mesosphere
with high vertical resolution.
Ueno says that once
aerosols are
in the
stratosphere they become very stable and can last for years, compared
with days or weeks
in the troposphere, and they can activate compounds such as chlorine that destroy the ozone layer.
Sulphur dioxide reacts
with water vapour to form long - lived droplets (
aerosols) of sulphuric acid, and about 10 million tons of these droplets are known to have accumulated
in the
stratosphere as a result of the eruption.
Rough calculations show if you drill about a dozen mine shafts as deep as possible into the thing, and plunk megaton nuclear bombs down there, and then fire them off simultaneously, you'll get a repeat of the Long Valley Caldera explosion of about 800,000 years ago — which coated everything east of it
with miles of ash and injected a giant
aerosol cloud into the
stratosphere — the ash layer alone formed a triangle stretching from the caldera to Louisiana to North Dakota, including all of Arizona and most of Idaho and everything
in between — I bet that would have a cooling factor of at least -30 W / m ^ 2 — and you could go and do the Yellowstone Plateau at the same time — geoengineering at its finest.
Ozone climatology: Some chemistry /
aerosol models will run
with interactive stratospheric chemistry while others will prescribe ozone
in the
stratosphere and only run
with detailed tropospheric chemistry.
This is similar to what happens
with industrial
aerosols: they never reach the
stratosphere and are washed away
in 1 - 2 weeks (Ramanathan).
Despite differences
in volcanic
aerosol parameters employed, models computing the
aerosol radiative effects interactively yield tropical and global mean lower - stratospheric warmings that are fairly consistent
with each other and
with observations (Ramachandran et al., 2000; Hansen et al., 2002; Yang and Schlesinger, 2002; Stenchikov et al., 2004; Ramaswamy et al., 2006b); however, there is a considerable range
in the responses
in the polar
stratosphere and troposphere.
Here, gasses react
with water to form
aerosol particles that linger
in the
stratosphere for one or two years, reflecting sunlight and heat from the sun, and cooling the planet.
One recent study estimated it would take 6,700 business jet flights per day — outfitted
with spraying equipment — to keep enough
aerosols in the
stratosphere to cool the climate by one degree Celsius.
Tinkering
with the Earth and its atmosphere
in an attempt to fend off global warming — a.k.a. geoengineering — seems like the stuff of science fiction: Lacing the
stratosphere with sulfur
aerosols or whitening clouds over the ocean to reflect sunlight back into space.
What does seem to be known is that
aerosols fall out of the lower atmosphere (as high as they can be launched
with conventional bombs)
in days, and persist for less than 2 years when launched into the
stratosphere by a major volcanic event like Pinatubo which was equivalent to several H bombs.
During this period, the
aerosol amount varied
with dust export from Africa, but also from major eruptions by two volcanoes (El Chichon
in 1982 and Pinatubo
in 1991), each of which left a reflective layer of sulfate droplets
in the lower
stratosphere for a couple of years.