CAUSES OF GREENHOUSE EFFECT
GREENHOUSE EFFECT
The greenhouse effect is a natural process that
warms the Earth’s surface. When the Sun’s energy reaches the Earth’s
atmosphere, some of it is reflected back to space and the rest is absorbed and
re-radiated by greenhouse gases.
Greenhouse gases include water vapour, carbon
dioxide, methane, nitrous oxide, ozone and some artificial chemicals such as
chlorofluorocarbons (CFCs).
The absorbed energy warms the atmosphere and
the surface of the Earth. This process maintains the Earth’s temperature at
around 33 degrees Celsius warmer than it would otherwise be, allowing life on
Earth to exist.
CAUSES OF THE
GREENHOUSE EFFECT
1. Burning
of Fossil Fuels: Fossil fuels
like coal, oil and natural gas have become an integral part of our life. They
are used on large basis to produce electricity and for transportation.
When they are burnt, the carbon stored inside them is released
which combines with oxygen in the air to create carbon dioxide. With the
increase in the population, the number of vehicles have also increased and this
has resulted in increase in the pollution in the atmosphere. When
these vehicles run, they release carbon dioxide, which is one the main gas
responsible for increase in greenhouse effect.
2. Deforestation: Forests hold a major green area
on the planet Earth. Plants and trees intake carbon dioxide and release oxygen,
through the process of photosynthesis, which is required by humans and animals
to survive. Large scale development has resulted in cutting down of trees
and forests which has forced people to look for alternate places for
living. When the wood is burnt, the stored carbon in converted back into carbon
dioxide.
3. Farming: Nitrous oxide is one the greenhouse
gas that is used in fertilizer and contributes to greenhouse effect which in
turn leads to global warming.
4. Industrial Waste and Landfills: Industries
which are involved in cement production, fertilizers, coal mining activities,
oil extraction produce harmful greenhouse gases. Also, landfills filled
with garbage produce carbon dioxide and methane gas contributing significantly
to greenhouse effect.
One of the reasons why our planet is able to
sustain life is because of the presence of greenhouse gases and their effect on
earth’s atmosphere and human beings. They can be summarized as follows:
· The
greenhouse effect maintains a manageable temperature on the earth’s surface and
makes it habitable for humans, plants and animals.
· The
greenhouse gases act as a filter. Unwanted solar energy is sent back to space.
Ozone absorbs the harmful ultraviolet rays of the sun. Carbon dioxide and other
gases absorb the longer wavelength radiation. Without these greenhouse gases
acting as filter, all harmful rays would have been radiated back to the earth’s
surface.
· For
ages, humans have used the greenhouse effect to grow plants even if it is not
the season for it. Out of season crops are grown by creating a greenhouse
effect artificially.
· Since
greenhouse gases helps to maintain the temperature, the primary effect of the
increase in greenhouse gases would be on climate. This would mean warmer
summers with natural disasters. Hurricanes have become common in recent years.
· Water
level balance of the earth would be destroyed. Polar ice caps would melt
leading to an increase in the ocean level. Floods will inundate low lying
areas.
· Marine
life and ecosystem would be destroyed. Oceans absorb carbon dioxide thereby affecting
the level of alkalinity. Many forms of marine life would be adversely affected
if alkalinity increases. Polar ecosystems would be destroyed. In the Arctic,
melting polar caps are threatening the habitats of polar bears and penguins.
· Global
warming would also affect the weather pattern. Rainfall would become erratic in
many parts of the world. This might eventually lead to desertification.
Overall the
impact of increased greenhouse effect on climate and human life would be
disastrous. The world community therefore needs to wake up now before it is too
late.
see also: causes-and-effects-of-climate-change
EFFECTS OF GREENHOUSE EFFECT
Global warming
Greenhouse gas
levels have been increasing since the start of the Industrial Revolution, but
over the last few decades growth has been particularly fast. Total greenhouse
gas emissions have increased by about 80% since 1970, creating a radiative
forcing of 2838 mW/m^2 equivalent to an atmospheric concentration of 473 ppm
CO2e.
Ocean Acidification
Increases in
carbon dioxide levels have made the world's oceans 30% more acidic since the
Industrial Revolution. The ocean serves as a sink for this gas and absorbs
about a quarter of human carbon dioxide emissions, which then goes on to
react with seawater to form carbonic acid. So as the level of carbon
dioxide in the atmosphere rises, the acidification of the oceans increases.
Changes to plant growth and nutrition levels
Since plants
need carbon dioxide to grow, if there are higher amounts in the air, plant
growth can increase. Experiments where carbon dioxide concentrations were
raised by around 50% increased crop growth by around 15%. Higher levels of
carbon dioxide makes carbon more available, but plants also need other
nutrients (like nitrogen, phosphorus, etc.) to grow and survive. Without
increases in those nutrients as well, the nutritional quality of many plants
will decrease. In different experiments with elevated carbon dioxide levels,
protein concentrations in wheat, rice, barley, and potato tubers, decreased by
5-14%.
Can the greenhouse effect be reversed?
Many
scientists agree that the damage to the Earth's atmosphere and climate is past
the point of no return or that the damage is near the point of no return.
"I agree that we have passed the point of avoiding climate change,"
Josef Werne, an associate professor at the department of geology &
planetary science at the University of Pittsburgh told Live Science. In Werne's
opinion, there are three options from this point forward:
1.
Do nothing and live with the consequences.
2.
Adapt to the changing climate (which includes
things like rising sea level and related flooding).
3.
Mitigate the impact of climate change by
aggressively enacting policies that actually reduce the concentration of CO2 in the atmosphere.
Keith Peterman,
a professor of chemistry at York College of Pennsylvania, and Gregory Foy, an
associate professor of chemistry at York College of Pennsylvania, think that
the damage isn't to that point yet, and that international agreements and
action can save the planet's atmosphere.
Currently, some
scientists are investigating how to re-engineer the atmosphere to reverse
global warming. For example, theories published in the journal Science in July
2017 by lrike Lohmann and Blaž Gasparini, researchers at the Institute of
Atmospheric and Climate Science at ETH Zurich in Switzerland, proposed reducing
cirrus clouds that trap heat.
"If cirrus clouds behave like a blanket
around the Earth, you're trying to get rid of that blanket," Lohmann, a
professor of experimental atmospheric physics at ETH Zurich, told Live Science.
[Cool the Planet? Geoengineering Is Easier Said Than Done]
"You remove the water vapor, you remove the humidity and you prevent the
normal cirrus cloud formation," Lohmann said.
References
1.
"Annex II Glossary".
Intergovernmental Panel on Climate Change. Retrieved 15 October 2010.
2.
Vaclav Smil (2003). The Earth's Biosphere:
Evolution, Dynamics, and Change. MIT Press. p. 107. ISBN 978-0-262-69298-4.
3.
IPCC AR4 WG1 (2007),
Solomon, S.; Qin, D.; Manning, M.; Chen, Z.; Marquis, M.; Averyt, K.B.; Tignor,
M.; Miller, H.L., eds., Climate Change 2007: The Physical Science Basis,
Contribution of Working Group I to the Fourth
Assessment Report of the Intergovernmental Panel on Climate
Change, Cambridge University Press, ISBN 978-0-521-88009-1 (pb: 978-0-521-70596-7)
4.
Schroeder, Daniel V. (2000). An
introduction to thermal physics. San Francisco,
California: Addison-Wesley. pp. 305–7. ISBN 0-321-27779-1. ...
this mechanism is called the greenhouse effect, even though most
greenhouses depend primarily on a different mechanism (namely, limiting
convective cooling).
5.
Wood, R.W. (1909). "Note on the
Theory of the Greenhouse". Philosophical Magazine. 17:
319–320. doi:10.1080/14786440208636602. When
exposed to sunlight the temperature rose gradually to 65 °C., the
enclosure covered with the salt plate keeping a little ahead of the other
because it transmitted the longer waves from the Sun, which were stopped by the
glass. In order to eliminate this action the sunlight was first passed through
a glass plate." "it is clear that the rock-salt plate is capable of
transmitting practically all of it, while the glass plate stops it entirely.
This shows us that the loss of temperature of the ground by radiation is very
small in comparison to the loss by convection, in other words that we gain very
little from the circumstance that the radiation is trapped.
6.
John Tyndall, Heat considered as a Mode
of Motion (500 pages; year 1863, 1873)
7.
Isaac M. Held; Brian J. Soden (Nov
2000). "Water Vapor Feedback and Global Warming". Annual
Review of Energy and the Environment. Annual Reviews. 25:
441–475. doi:10.1146/annurev.energy.25.1.441.
8.
Easterbrook, Steve. "Who first coined
the term "Greenhouse Effect"?". Serendipity.
Retrieved 11 November 2015.
9.
Ekholm N (1901). "On The Variations
Of The Climate Of The Geological And Historical Past And Their
Causes". Quarterly Journal of the Royal Meteorological Society. 27(117):
1–62. Bibcode:1901QJRMS..27....1E. doi:10.1002/qj.49702711702.
10.
"NASA Earth Fact Sheet". Nssdc.gsfc.nasa.gov.
Retrieved 2010-10-15.
11.
"Introduction to Atmospheric Chemistry, by
Daniel J. Jacob, Princeton University Press, 1999. Chapter 7, "The
Greenhouse Effect"". Acmg.seas.harvard.edu. Retrieved 2010-10-15.
12.
"Solar Radiation and the Earth's Energy
Balance". Eesc.columbia.edu. Retrieved 2010-10-15.
14.
The elusive "absolute surface air
temperature," see GISS discussion
15.
Mitchell, John F. B. (1989). "THE "GREENHOUSE" EFFECT AND CLIMATE
CHANGE" (PDF). Reviews of Geophysics. American
Geophysical Union. 27 (1): 115–139. Bibcode:1989RvGeo..27..115M. doi:10.1029/RG027i001p00115.
Retrieved 2008-03-23.
16.
"Water vapour: feedback or forcing?".
RealClimate. 6 April 2005. Retrieved 2006-05-01.
17.
Kiehl, J. T.; Kevin E. Trenberth (February
1997). "Earth's Annual Global Mean Energy Budget" (PDF). Bulletin
of the American Meteorological Society. 78 (2): 197–208. Bibcode:1997BAMS...78..197K. doi:10.1175/1520-0477(1997)078<0197:EAGMEB>2.0.CO;2. ISSN 1520-0477.
Archived from the original (PDF) on 2006-03-30.
Retrieved 2006-05-01
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