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Why can one volcanic eruption produce more deadly
gases than all the emissions of every car that has
ever been used. And why is the average temperature
of the earth getting colder? |
Question Date: 2013-06-29 | | Answer 1:
We measure the magnitude of a volcanic
eruption by the total mass that erupts. For
example, an eruption, a super eruption may have a
volume of 1000 km3. Now since the
density of magma is about 2000 kg.m3,
the total mass of one of these super eruptions is
equal to the product of the density times the
volume. If we use consistent SI units then that
gives a mass of 2x1015 kg of magma. Now
the gas content of a typical magma is circa 2 wt %
; most of that is H2O and
CO2 and Sulfur gasses.
On the order of 0.1 wt %is CO, H2S
and other rather toxic gasses. Some of these gas
components are oxidized when erupted. So if we say
that 0.1 wt % of the total mass is toxic gas, then
a super eruption expel on the order of
2x1012 kg is noxious gas!
How it compares with the noxious gas of all the
cars emit in Los Angeles (for example) over the
years, I am not sure. Maybe you can look that up
and compare.
| | Answer 2:
Actually, the first statement is misleading and
the second statement is not true.
While volcanoes emit poisonous fumes that
originate from dissolved gases in the Earth's
magma, these poisonous gases are only part of the
concern associated with human activity.
CO2 and other "greenhouse gases" are
what I would imagine are of greater concern. Every
year, human activities emit around 100 times more
CO2 than volcanoes do in the same
period of time (30 billion tons vs. 30 million
tons -- to put it another way, 30,000,000,000 vs
300,000,000 tons -- that is A LOT of
CO2). The
amount of CO2 in the atmosphere is the
highest it has been in about 15 million years. 15
million years ago, temperatures were about 5-10
degrees warmer on average than they are now, the
sea levels were about 70-120 feet higher, and
there was no permanent sea ice cap in the Arctic.
Regarding the second question, the average
temperature on Earth has been getting warmer over
the past couple of centuries. There are natural
fluctuations that occur in the Earth's
temperature, but the main point of concern is the
levels of chemicals such as CO2 and
Non-Methane-Hydrocarbons ("NMHC's") in the
atmosphere. There is a very delicate balance of
reaction pathways in the atmosphere that in turn
are coupled to chemical reaction pathways in the
ocean and on land (i.e biogeochemical cycles).
Upsetting this balance by emitting a large amount
of these chemicals into the atmosphere can have
lasting and far-reaching consequences. One example
is that increased CO2 in the atmosphere
leads to increased CO2 in the ocean,
which in turn acidifies the ocean. Changing the pH
of the ocean changes which lifeforms can live
where or whether they can live at all. This
affects many foodchains in the ocean, some of
which humans are a part of. Furthermore,
pollutants can be taken up by some of the
organisms in the ocean and they can propagate up a
food chain and back to human predators.
| | Answer 3:
That is an interesting question. You are correct
that volcanoes release gases such as carbon
dioxide (CO2), hydrogen sulfide
(H2S), and sulfur dioxide
(SO2) into the atmosphere. It is not
clear to me which “deadly gases” you are referring
to. Cars are known to be major sources of
CO2, which is a powerful greenhouse gas
that has the affect of warming the global climate.
Cars and other anthropogenic (caused by humans)
sources of CO2 release MUCH more
CO2 into the atmosphere than present
day volcanoes.
Estimates for the amount of CO2
released by present day volcanoes range from
0.13–0.44 billion tons per year, while the
estimated anthropogenic CO2 emitted in
2010 was 35 billion tons (Friedlingstein, 2010;
Gerlach, 2011). That’s roughly 100 times more
CO2 coming from people than from
volcanoes.
Additionally, a large proportion of the
CO2 released from volcanoes is recycled
through the mantle of the earth (the layer below
the crust). One study of the gases from an island
arc volcano (like Japan or Sumatra) showed that
67% of the CO2 was sourced from
inorganic sedimentary carbon that was subducted
beneath the volcano (carried down on a sinking
ocean slab), and less than 12% was primordial
(from the mantle; representing net addition to the
atmosphere; Fisher et al., 1998).
There are indeed other gases (mentioned above)
that are sourced from volcanoes. Sulfur dioxide is
a gas that actually causes short-term (months to
years) global cooling as it forms aerosols in the
atmosphere. It forms sulfuric acid in the
atmosphere, causing acid rain. To my knowledge,
not much SO2 is produced by cars, but
huge amounts are generated from other
anthropogenic sources like coal power plants.
In summary, volcanoes do emit gases that can
have adverse affects on our climate, ecosystems,
and health, but the scale is much smaller than
that produced by humans. It is important to keep
in mind (this is personal opinion, not scientific
observation) that gas releases from volcanoes is a
natural process! This process has been going on
for billions of years and has reached a sort of
long-term equilibrium; the concentration of
different gases does indeed fluctuate up and down
on scales of thousands and millions of years. The
affect that humans have had on the climate
(especially over the last couple hundred years) is
much more rapid and causes conditions that are
harmful to some of our societal infrastructures.
As an example, check out the discussion on recent
severe weather (hurricanes, tornadoes, etc.). I am
not saying that recent intense storms are
definitely caused by anthropogenic climate change,
but it is an interesting debate. Be cautious about
the sources that you use for research. Peer
reviewed journal articles are those that have been
checked by other experts in the field before being
published. That does not mean that they are never
biased, but it generally ensures that only the
“good science” makes it to press.
And why is the average temperature of the
earth getting colder?
Please read the answer #4 below | | Answer 4:
And why is the average temperature of the
earth getting colder?
I am a little unclear about what this question is
asking. The average temperature of the entire
earth (the crust, mantle, and core) is getting
colder, but the average temperature of the
atmosphere is getting warmer. The solid part of
the earth has steadily cooled down over billions
of years as it loses heat generated during the
formation of the planet and the decay of
radioactive elements like potassium, uranium, and
thorium.
The atmosphere, which is a major part of global
climate, has been getting warmer at a very fast
rate over the last hundred years or so. The figure
below shows a global temperature anomaly curve for
the time period between 1880–2005 (Hansen et al.,
2006).
average-temperature
The “temperature anomaly” is relative to the
temperature between 1951 and 1980. A positive
anomaly indicates a time that when the temperature
was higher than this period, a negative anomaly
indicates a time that was colder. The graph shows
that temperature has increased rapidly (up to 0.6
C more than between 1951 and 1980). You can see
that there are little up and down jumps in this
curve. There are changes in the mean global
temperature (both up and down) that happen on a
very short term (several years), and there is also
some uncertainty around the values that were used
to construct this curve, but the trend of
increasing temperature is obvious.
I apologize if your question was about the
cooling of the solid earth over geologic time and
not the warming of the atmosphere caused by
humans. I may have missed the mark.
References
Fisher, T.P. et al. (1998). Fluxes and sources of
volatiles discharged from Kudryavy, a subduction
zone volcano, Kurile Islands. Earth and Planetary
Science Letters, 160, 81–96.
Friedlingstein, P.et al. (2010). Updated on
CO2 emissions. Nature Geoscience, 3,
811–812.
Gerlach, T. (2011). Volcanic versus anthropogenic
carbon dioxide. EOS, Transactions, American
Geophysical Union, 92, 201–208.
Hansen, J. et al. (2006). Global temperature
change. Proceedings of the National Academy of
Sciences, 103, 14288–14293.
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