These intervals are often analyzed
for volcanic sulfate by ice core scientists.
Not exact matches
To determine whether declining pollutants deserve credit
for the recovery, the researchers used a 3D atmospheric model to separate the effects of the chemicals from those of weather, which can affect ozone loss through winds and temperature, and
volcanic eruptions, which deplete ozone by pumping
sulfate particles into the upper atmosphere.
Recent inspection of the
sulfate records from the European project
for ice coring in Antarctica's dronning maud land (EDML) ice core reveals
sulfate peaks that have been correlated to presumed YTT
sulfate peaks in the North Greenland ice core project (NGRIP) and GISP2 ice cores; however, once again no
volcanic material has been identified (18).
My idea of a thriller novel, with at least the plot potential of State Of Fear, has
for years been a group of rogue scientists who drill down to near the magma of a volcano on a remote Indonesian island and drop a nuclear bomb down there to break things loose and start a real
volcanic reaction — leaving us with lots of
sulfates in the atmosphere.
I also found a paper analyzing
sulfate from a different Greenland ice core
for volcanic eruption signals: http://epic.awi.de/Publications/Big2001a.pdf
Also,
volcanic eruptions such as that of the Philippines» Mt. Pinatubo in 1991 can cool the planet
for a few years by adding
sulfate particles into the stratosphere, reflecting solar radiation back to space.
Global solar irradiance reconstruction [48 — 50] and ice - core based
sulfate (SO4) influx in the Northern Hemisphere [51] from
volcanic activity (a); mean annual temperature (MAT) reconstructions
for the Northern Hemisphere [52], North America [29], and the American Southwest * expressed as anomalies based on 1961 — 1990 temperature averages (b); changes in ENSO - related variability based on El Junco diatom record [41], oxygen isotopes records from Palmyra [42], and the unified ENSO proxy [UEP; 23](c); changes in PDSI variability
for the American Southwest (d), and changes in winter precipitation variability as simulated by CESM model ensembles 2 to 5 [43].
Observed temperature (black line), the out - of - sample forecast
for global surface temperature driven by anthropogenic changes in radiative forcing (red line) and the out - of - sample forecast
for global surface temperature driven by natural variables (solar insolation, SOI, and
volcanic sulfates)(green line).
The 95 % confidence intervals in Figs. 2 and 3 represent uncertainty in the statistical estimates of the regression model
for observed paths of forcings, SOI, and
volcanic sulfates.
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.
Time series
for solar insolation (18), SOI (19), and the radiative forcing of
volcanic sulfates (20) are updated with values from sources that are used to generate the original dataset.
That same reference finds that the statistical estimates
for the temperature effect of
volcanic sulfates and ENSO (and effects of ENSO on atmospheric CO2) are consistent with estimates derived from climate models and empirical analyses.
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...