Besides knowing a lot more about the transport of
volcanic aerosols in the atmosphere, modern researchers had communications lines and satellites so that news of an eruption could be relayed quickly and the effects noted as they unfolded.
«We found that red - to - green ratios measured in the sunsets of paintings by great masters correlate well with the amount of
volcanic aerosols in the atmosphere, regardless of the painters and of the school of painting,» Zerefos said.
Not exact matches
Forcing caused by changes
in the Sun's brightness, by dust
in the
atmosphere, or by
volcanic aerosols can also be translated into radiative forcing.
In addition, since the global surface temperature records are a measure that responds to albedo changes (volcanic aerosols, cloud cover, land use, snow and ice cover) solar output, and differences in partition of various forcings into the oceans / atmosphere / land / cryosphere, teasing out just the effect of CO2 + water vapor over the short term is difficult to impossibl
In addition, since the global surface temperature records are a measure that responds to albedo changes (
volcanic aerosols, cloud cover, land use, snow and ice cover) solar output, and differences
in partition of various forcings into the oceans / atmosphere / land / cryosphere, teasing out just the effect of CO2 + water vapor over the short term is difficult to impossibl
in partition of various forcings into the oceans /
atmosphere / land / cryosphere, teasing out just the effect of CO2 + water vapor over the short term is difficult to impossible.
In addition, the later non-warming period also was a period of high
volcanic activity adding even more
aerosols to the
atmosphere.
Volcanic events and some types of human - made pollution, both of which inject sunlight - reflecting
aerosols (i.e., tiny particles) into the
atmosphere, lower temperature and are examples of forcings that drive decreases
in temperature.
If by observational data, you mean the amount of
aerosols in the
atmosphere, I think that would be a key piece of information that would need to be included
in the models as without it the response to
volcanic events can not be modeled or predicted.
These were intriguing, as well as highly speculative: first the possibility of deliberately using additional targeted
aerosol injection to stimulate coagulation of the particles
in the
volcanic aerosol; mitigating its effects by causing the particles to drop out of the
atmosphere more swiftly.
Some models include
volcanic effects by simply perturbing the incoming shortwave radiation at the top of the
atmosphere, while others simulate explicitly the radiative effects of the
aerosols in the stratosphere.
This is the portion of temperature change that is imposed on the ocean -
atmosphere - land system from the outside and it includes contributions from anthropogenic increases
in greenhouse gasses,
aerosols, and land - use change as well as changes
in solar radiation and
volcanic aerosols.
This cooling was from the same root cause as
volcanic cooling, namely
aerosols (mostly sulfate
aerosols)
in the
atmosphere.
Causes, and they are multiple, appear to be: 1) Natural variability of ocean to
atmosphere sensible and latent heat flux 2) Modest increase
in natural
volcanic aerosols 3) Slight decrease
in solar output
12 * ICE AGES: More elliptical orbit causes less sunlight to reach Earth — results
in ice ages (100,000 yr cycles) *
VOLCANIC ACTIVITY: Release ash and
aerosols into the
atmosphere Reflects sun rays causing cooler temps * SOLAR ENERGY: Cause short term changes Less solar energy can cause small ice ages
However, over long time periods, the variation of the global average temperature with CO2 concentration depends on various factors such as the placement of the continents on Earth, the functionality of ocean currents, the past history of the climate, the orientation of the Earth's orbit relative to the Sun, the luminosity of the Sun, the presence of
aerosols in the
atmosphere,
volcanic action, land clearing, biological evolution, etc..
Aerosols emitted for only a short time would have minimal effects that subside very quickly.The industrial aerosols are rich in SO2, while apparently, the Chilean volcanic eruption did not (according the news item) spew enough SO2 into the atmosphere for discernible climate
Aerosols emitted for only a short time would have minimal effects that subside very quickly.The industrial
aerosols are rich in SO2, while apparently, the Chilean volcanic eruption did not (according the news item) spew enough SO2 into the atmosphere for discernible climate
aerosols are rich
in SO2, while apparently, the Chilean
volcanic eruption did not (according the news item) spew enough SO2 into the
atmosphere for discernible climate effects.
Aerosols from
volcanic eruptions do have a cooling effect once they reach the stratosphere but the effect of high wind speed
in the upper
atmosphere would rapidly disperse these, and any local effects would be very slight.
Previous pauses
in temperature rise
in 1982 and 1991 were attributed to the ash and sulfur
aerosols spewed into the
atmosphere by the
volcanic eruptions of El Chichón
in Mexico and Pinatubo
in the Philippines, respectively.
The results suggested that moderate
volcanic eruptions were behind the increases of
aerosols in the
atmosphere.
Turner's work,
in particular, which often depicts brightly colored sunsets and emphasized natural light, can be used to roughly estimate
aerosol optical depth — that is, the amount of particles like dust,
volcanic ash, smoke and sea salts
in the
atmosphere — at the time the painting was made.
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 negligible.
Sulfur dioxide is an
aerosol that forms droplets of sulphuric acid
in the high
atmosphere and reflects solar energy back into space, so these two
volcanic eruptions had some short - to medium - term effects.
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.
The global temperature rise during the ETCW implies a change
in the energy budget of the Earth's
atmosphere, which
in turn suggests either an external forcing (
volcanic, solar, greenhousegases, tropospheric
aerosols), changes
in clouds, or ocean heat release (Brönnimann, 2015b).
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...
DePreSys (18) takes into account the observed state of the
atmosphere and ocean
in order to predict internal variability, together with plausible changes
in anthropogenic sources of greenhouse gases and
aerosol concentrations (19) and projected changes
in solar irradiance and
volcanic aerosol (20).