Global
cooling after volcanic eruptions has been recorded in ice core data and thermometers,: 1809, 1815, 1883, 1980 etc. and others.
Not exact matches
After large
volcanic eruptions that pump sulphur dioxide into the atmosphere, such as that of mount Pinatubo in the Philippines in 1991, the planet
cools for a year or two.
Besides SSCE, scientists have also been investigating stratospheric sulfur injections — firing sun - reflecting aerosols into the air, similar to the
cooling effect
after a
volcanic eruption — and cirrus cloud thinning, where you thin the top level of clouds, which have a warming effect on the planet.
Researchers know that large amounts of aerosols can significantly
cool the planet; the effect has been observed
after large
volcanic eruptions.
Not until
after a catastrophic chain of
volcanic eruptions cooled the Earth and decimated those competitors did dinosaurs become dominant worldwide.
It's also now well understood that large
volcanic eruptions have a short - term
cooling effect, see GW FAQ: effect of
volcanic activity (short - term being the key phrase,
after Church et al Nature 2005, and also http://www.llnl.gov/str/JulAug02/Santer.html)
The short - term variations are dominated by ENSO but also can be influenced by large tropical
volcanic eruptions (such as occurred in 1963, 1982 and, markedly, 1991), so the years
after those
eruptions are anomalously
cool.
(For instance, do the models predict
cooling after big
volcanic eruptions?
In other words, if we are
after a cause (or causes) for the temperature increase during the period in question, the presence or absence of aerosols from
volcanic eruptions is beside the point, because they can not explain any increase in temperatures that occurred prior to any
cooling effect they might have had.
Some longer - term effects may remain
after several consecutive
eruptions, but even then, the 0.1 K
cooling by
volcanic eruptions over the past 600 years (0.3 K modeled over the past 100 years, see fig. 1 on this page) seems rather high...
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.
Volcanic activity was high during this period of history, and we know from modern studies of volcanism that
eruptions can have strong
cooling effects on the climate for several years
after an
eruption.
He writes: I say this is a result of the action of climate phenomena that oppose the
cooling... if my theory were correct, we should see a
volcanic signal in some other part of the climate system involved in governing the temperature... I should see an increase in the heat contained in the Pacific Ocean
after the
eruptions Thing is, El Ninos release heat from the ocean, they don't store heat.
In fact, the rate of change of CO2 levels actually drops slightly
after a
volcanic eruption, possibly due to the
cooling effect of aerosols.
In effect, these particles — whether aerosols or kitchen table salt — could act like natural aerosols that
cool the planet
after a
volcanic eruption.
[Using the GISS record staring in 1991 or 1992 — the
cool years just
after the
volcanic eruption of Mt. Pinatubo]
Generally, a significant
cooling of the surface occurs in the first weeks
after major
volcanic eruptions, lasting for one to two years and leading to modified patterns of precipitation, surface pressure and the teleconnection patterns, such as the Arctic Oscillation (AO), North Atlantic Oscillation (NAO)
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.
The short - term variations are dominated by ENSO but also can be influenced by large tropical
volcanic eruptions (such as occurred in 1963, 1982 and, markedly, 1991), so the years
after those
eruptions are anomalously
cool.
Third: There was no
cooling in the 1920s; in fact that was the start of a multidecadal warming trend that lasted until just
after World War II (followed by a brief
cooling trend, possibly due to increased aerosols dimming incoming sunlight together with some pretty big
volcanic eruptions which did the same thing).
Observations of recent global warming, short - term
cooling after major
volcanic eruptions,
cooling at the Last Glacial Maximum and other periods in the historical record, and the seasonal variation in climate, all provide some information which helps to determine the value of climate sensitivity.
We'd expect to see the imprint of this large error in comparisons with observed surface temperature changes over the 20th century (37 - 42), and in comparisons with the observed
cooling after large
volcanic eruptions (30, 43, 44).