The Greenhouse Effect

Running Head: THE GREEN HOUSE EFFECT 1
The Greenhouse Effect
Name:
Institutional affiliation;
Course:
Instructor:
THE GREENHOUSE EFFECT
2
The Greenhouse Effect
Introduction
Greenhouse effect generally refers to a phenomenon where thermal radiation from the
earth’s surface is absorbed by the greenhouse gases in the atmosphere and then re-radiated
back. The re-radiation effect causes the temperature on the earth surface to be higher than
what it would be if these atmospheric gases were absent. A larger proportion of infrared
radiation being reflected upward form the surface of the earth is absorbed in the atmosphere
and re-radiated (reflected) upward and downward. What makes the atmosphere much warmer
than it would be is the fact that, the earth’s surface does not just receive solar radiation but, in
addition receives infra-red radiation from, the clouds and the atmosphere. This mechanism is
named after the actual greenhouses where the solar radiation passes through a glass or
polythene warming the greenhouse. The way greenhouse retains heat is a little different as it
mostly works by restricting the upward convection of heat but not radiation. The greenhouse
effect is responsible for making the earth warm. Without this effect, the earth would be colder
and inhabitable (Sorokhtin, Chillinger&Khilyuk, 2007).
Water vapor is one most important atmospheric greenhouse gases. Water vapor plays
a major function in holding the outgoing terrestrial radiation. However, the water vapor is not
treated as an external force in the climate system, but as feedback since it responds rapidly
according to the changing climatic conditions. Clouds and water vapor play a very important
role as the climate system feedbacks.
Apart from the water vapor, the very important greenhouse gases (which are highly
emphasized) include carbon dioxide, organic gases (methane), ozone, nitrous oxide and
chlorofluorocarbons (CFCs). The chlorofluorocarbons are totally from anthropogenic source.
Carbon dioxide is believed to be responding to changes and sinks from forty to hundreds of
THE GREENHOUSE EFFECT
3
years whereas methane inherent scale of time is about eight years. The ozone, which
concentrates more in the middle stratosphere, filters the harmful ultraviolet radiation. The
percentage of these greenhouse gases in the atmosphere is less than one. The concentration of
these gases is controlled by ‘sources’ and ‘sinks’ processes. These are processes are involved
in the generation and destruction of greenhouse gases respectively. Human affects the levels
of greenhouse gases through the introduction of new sources and interference of the natural
sinks. By interfering with the natural trend of these gases, it will result to increased intensity
of global warming; a condition where there are increases in the temperature on the earth.
Alongside fossil fuel gases, carbon dioxide is one of the most highlighted greenhouse
gases. The concentration of carbon dioxide in the atmosphere has been rising since the 19th
century (Keller, 2007). Human activities such as deforestation and utilization of fossil fuels
contribute to this rise. Its level is anticipated to double the natural postglacial value in the
coming years if the no measures are taken to control it. According to the National Oceanic
and Atmospheric Administration (NOAA) the current atmospheric CO2 levels stand at
approximately 400 parts per million (PPM), This is an increase of about 30% since 1860
(using www.esrl.noaa.gov, 2014. ) The factors that have contributed to this rise in carbon
dioxide include industrialization and deforestation in the advancement of settlement to
contain the growing population. The industries consume fossil fuels and result in emitting
significant amounts of CO2 in the atmosphere. This shows how the industrial revolution since
mid 19th century has contributed to rise in atmospheric carbon dioxide. More on this, there
has been a very sharp increase in the number of automobiles which emit CO2 alongside other
greenhouse gases to the atmosphere. Cutting down of vegetation to create room for
urbanization and for commercial purposes has also been on the rise. Vegetation play a crucial
role in controlling of atmospheric carbon dioxide hence man destroys them the CO2 levels
increases.
THE GREENHOUSE EFFECT
4
Having analyzed the evidence of the relationship between the increase in carbon
dioxide concentrations and temperatures much has been predicted. It is predicted that more
violent atmospheric disturbances (storms) will be experienced due to thermal energy increase
in the atmosphere. Other predictions that relate to not reducing the rate of these emissions
include an increase in global temperatures, rise in sea levels, inundation of islands and sea
levels and shift of climate zones. All these create an event known as climate change. It is also
predicted that a lot of diseases will spread to the temperate regions from the tropics where
disease-causing insects thrive.
The scientists and researchers agree that emitting more greenhouse gases such as
carbon dioxide will raise the earth’s temperatures and result to negative effects (Keller,
2007). How much and how soon this will happen, is still a debatable issue. There is
uncertainty in the whole issue because of complexities of the climate system hence making it
hard to predict. Before acting to these predictions, it is important to be certain about the
extents and disparities of these phenomena. The policymakers must work hand in hand with
the scientists and clear the air about the real issues of climate change. This will help come up
with an implementable plan of action to deal with the problem, instead of relying on
objectionable predictions.
THE GREENHOUSE EFFECT
5
References
ESRL Global Monitoring Division - Global Greenhouse Gas Reference Network.(n.d.).ESRL
Co2 Trends RSS. Retrieved March 6, 2014, from
http://www.esrl.noaa.gov/gmd/ccgg/trends/
Jakab, C. (2011). Greenhouse gases. New York: Marshall Cavendish Benchmark.
Keller, C. F. (2007). Global Warming 2007. An Update to Global Warming: The Balance of
Evidence and Its Policy Implications. TheScientificWorldJournal, 7, 381-399.
Shukla, J. S. (2013). Question Mark on Earth in Context of Green House Effect.IOSR Journal
Of Environmental Science, Toxicology And Food Technology, 4(4), 38-46.
Sorokhtin, O. G., Chilingar, G. V., &Khilyuk, L. F. (2007).Global warming and global
cooling evolution of climate on Earth..S.l.: Elsevier Science.

Place new order. It's free, fast and safe

-+
550 words

Our customers say

Customer Avatar
Jeff Curtis
USA, Student

"I'm fully satisfied with the essay I've just received. When I read it, I felt like it was exactly what I wanted to say, but couldn’t find the necessary words. Thank you!"

Customer Avatar
Ian McGregor
UK, Student

"I don’t know what I would do without your assistance! With your help, I met my deadline just in time and the work was very professional. I will be back in several days with another assignment!"

Customer Avatar
Shannon Williams
Canada, Student

"It was the perfect experience! I enjoyed working with my writer, he delivered my work on time and followed all the guidelines about the referencing and contents."

  • 5-paragraph Essay
  • Admission Essay
  • Annotated Bibliography
  • Argumentative Essay
  • Article Review
  • Assignment
  • Biography
  • Book/Movie Review
  • Business Plan
  • Case Study
  • Cause and Effect Essay
  • Classification Essay
  • Comparison Essay
  • Coursework
  • Creative Writing
  • Critical Thinking/Review
  • Deductive Essay
  • Definition Essay
  • Essay (Any Type)
  • Exploratory Essay
  • Expository Essay
  • Informal Essay
  • Literature Essay
  • Multiple Choice Question
  • Narrative Essay
  • Personal Essay
  • Persuasive Essay
  • Powerpoint Presentation
  • Reflective Writing
  • Research Essay
  • Response Essay
  • Scholarship Essay
  • Term Paper
We use cookies to provide you with the best possible experience. By using this website you are accepting the use of cookies mentioned in our Privacy Policy.