Not exact matches
Since the 1990s, scientists have been discussing using aircraft to inject
aerosols, such as
sulfates, into the atmosphere as a form of geoengineering to mimic
volcanic eruptions that sometimes cool the planet by casting shades of particulate matter.
A third key hypothesis involves acidic
aerosols released at
volcanic sites, such as acid fog, dispersed throughout the atmosphere, and interacting subsequently with the finer components of soil as a source of widespread hydrated iron -
sulfate salts.
Like the particles emitted during
volcanic eruptions,
sulfate aerosols cool the Earth by blocking a portion of the sun's rays.
Volcanoes can — and do — influence the global climate over time periods of a few years but this is achieved through the injection of
sulfate aerosols into the high reaches of the atmosphere during the very large
volcanic eruptions that occur sporadically each century.
-LSB-...] following a major
volcanic eruption (emitting
sulfate aerosol in the stratosphere).
After a large
volcanic eruption, the layer of
sulfate aerosols in the stratosphere gets thicker, and we see, in the historic record, that the Earth cools down in response.
In fact, the major effect of significant
volcanic eruptions is cooling due to the
sulfate aerosols that they release (although in order to have a significant cooling effect, the eruption has to be large enough that it injects the
aerosols into the stratosphere where they can stay around longer... and it apparently helps if the eruption is reasonably near to the equator).
This cooling was from the same root cause as
volcanic cooling, namely
aerosols (mostly
sulfate aerosols) in the atmosphere.
Volcanoes can — and do — influence the global climate over time periods of a few years but this is achieved through the injection of
sulfate aerosols into the high reaches of the atmosphere during the very large
volcanic eruptions that occur sporadically each century.
10 Heat Storage: Mostly the Oceans 1955 - 1996; Levitus et al. 2001: Science World Ocean = 18.2 x10 22 Joules Atmosphere = 0.7 x10 22 Joules Land Ice = 0.8 x10 22 Joules observed Modeled Model includes forcing from Greenhouse Gases,
Sulfate Aerosols Solar irradiance changes, and volcanic a
Aerosols Solar irradiance changes, and
volcanic aerosolsaerosols.
That is contradicted by climate models providing a very decent match to the observed cooling following a major
volcanic eruption (emitting
sulfate aerosol in the stratosphere).
The
Sulfate cooling mechanism is also evidenced whenever there is a high ejecta mass volcanic eruption, which causes a measurable cooling effect, for about 3 years after an eruption; until the sulfate particulate aerosols diminish in the atmosphere to the point that they become negl
Sulfate cooling mechanism is also evidenced whenever there is a high ejecta mass
volcanic eruption, which causes a measurable cooling effect, for about 3 years after an eruption; until the
sulfate particulate aerosols diminish in the atmosphere to the point that they become negl
sulfate particulate
aerosols diminish in the atmosphere to the point that they become negligible.
But to quantify the influences (or «forcings» in climate jargon) even further, they considered three anthropogenic forcings — well - mixed greenhouse gases,
sulfate aerosols, and tropospheric and stratospheric ozone — as well as two natural forcings — changes in solar irradiance and
volcanic aerosols — all of which are likely to influence tropopause height.»
Volcanic eruptions emit sulfate aerosols via volcanic plumes, which may stay in the stratosphere for months to years, reflecting sunlight back into space, cooling the Earth's lower atmosphere or troposphere over a long
Volcanic eruptions emit
sulfate aerosols via
volcanic plumes, which may stay in the stratosphere for months to years, reflecting sunlight back into space, cooling the Earth's lower atmosphere or troposphere over a long
volcanic plumes, which may stay in the stratosphere for months to years, reflecting sunlight back into space, cooling the Earth's lower atmosphere or troposphere over a long time...