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.


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, CaliforniaAddison-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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