GUIDED BY-
Dr. JAMESMATTHEW
SUBMITTED BY-
NEHA MISHRA
(M.Sc. 4TH sem.)
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 Greenhouse a building made mainly of glass, with
heat & humidity regulated for growing plants. The
atmosphere acts like a glass in a greenhouse.
 Atmosphere, like glass absorbs some of the long
wave radiation emitted by earth and radiates the
energy back to earth. In this way temperature of
earth is maintained.
 The atmosphere surrounding the earth in this
manner plays a vital role in maintaining an even
temperature on the earth’s surface.
 A greenhouse is that body which allows the short
wavelength incoming solar radiation to come in, but
does not allow the long wave outgoing terrestrial
infrared radiation to escape.
 Earth’s atmosphere bottles up the energy of the sun, &
is said to act like a greenhouse.
 Carbon-dioxide present in the atmosphere acts like
glass windows.
 Carbon-dioxide and water vapours in the atmosphere
transmit short wavelength solar radiation but reflect the
longer wavelength heat radiation from warmed surface
of the earth.
 Carbon-dioxide molecules are transparent to sunlight
but not but not to the heat radiation.
 They trap the re-enforce the solar heat.
 The Greenhouse effect defined as the progressive
warming up of the earth’s surface due to blanketing
effect of manmade CO2 in the atmosphere.
 The four major greenhouse gases, which causes
adverse effects are carbon-dioxide, methane, nitrous
oxide and chlorofluorocarbon.
 For the earth, water vapour is the most important of all
greenhouse gases.
 Water vapour absorbs IR in the region 2.5 to 3.5 µm 5 to
7 µm, as well as over a broad range above 13 µm.
CARBON-DIOXIDE
 It is a major contributor to greenhouse effect because it
absorbs IR in the range of 14 to 19 µm, and completely
blocks the radiation flux between 15 to 16 µm.
 The burning of fossil fuels such as coal, tar, and natural
gases release CO2 . Burning of wood, waste materials
and tress release CO2.
METHANE
 Methane absorb radiation in the wavelength ranges
from 3 to 4 µm and 7 – 8.4 µm (in the window region).
 Methane gas increases stratospheric water vapour on
oxidation and the rise in water vapour is more important
source of greenhouse effect than the direct effect of
methane gas.
NITROUS OXIDE
 Nitrous oxide absorb IR radiation in the ranges 3 to 5
µm and 7.5 to 9 µm (infrared window).
 The major sources of nitrous oxide are microbial
denitrification, conversion of nitrate to nitrous oxide
soils, lake and oceans.
 Methane gas is 24 times & nitrous oxide is around 320
times aggressive greenhouse gas than carbon dioxide.
CHLOROFLUROCARBONS (CFCS)
 CFCs absorb in the range 8 to 12 µm with each CFC
having specific absorption bands in the region.
 CFCs are released into the atmosphere during the
operations and maintenances of appliances and
equipments using these molecules as coolants and
propellants.
HYDROCHLOROFLUROCARBONS (HCFCS)
 The HCFCs also attenuate radiation within the same
range, but their in the troposphere is much shorter than
that of the CFCs.
 The rate of increase of CFCs has declined by a factor
greater than two in the past decade, but HCFC
concentrations are increasing at a much higher rate.
The greenhouse effect will bring about the following important
changes in the climate of the Earth.
 As a result of rise in temperature of the earth due to
greenhouse effect the oceans get warm up and sea level
would rise flooding low lying regions.
 In temperate regions, the winter will be shorter and
warmer and the summer will be longer and hotter.
 There will be enormous increase in rainfall but the
problems of desertification, drought and soil erosion will
further worsen.
 The tropics may become wetter and the subtropics,
which are already dry, are expected to be drier.
 The plants & animals will also be affected resulting in the
disruption of the whole ecosystem.
 Erik M. Conway(2008) defined global warming as “the
increase in Earth’s average surface temperature due to
rising levels of greenhouse gases”.
 Global warming will lead to higher temperature and
changes in rainfall, and this in turn will modify the extent
and productivity of land suitable for agriculture.
• For example, a temperature increase of 3ºC paired with a
rainfall increase of 10% in the developing countries would
cause a decrease of 11% productivity that could have
serious consequences for food security.
 According to latest climate change report, global warming
would decrease crop production in developing countries
but increase in industrialised world.
 Global warming would also have short term and long term
effects on human health and environment.
 The hot days are sure to be scorching and cold ones
freezing.
 In future, the rain is going to be intensive.
 Changes in frequency & intensity of extreme weather will
have profound impact human society and natural
resources.
 A few study forecast an increase in the number of deep
cyclones and increase in intensity of the storm over
western Europe.
 With the continuing increase in greenhouse gases in the
21st century, the losses caused by natural calamites and
catastrophes are bound to increase.
 A century from now, the Earth’s surface will be about 3.5ºC
higher than in 1990.
 Surface ocean waters today are roughly 30
percent more acidic than at the start of the
Industrial Revolution.
 In the last decade, the rate of Antarctica's ice
mass depletion has tripled.
 Scientists predict that the Arctic Ocean will
barely have ice before 2050.
 For the last twenty years, sea levels rose at
twice their rate during the last century.
 Global temperatures could increase by as much
as 10.4 degrees Fahrenheit by 2100.
 https://www.britannica.com/science/global-warming
 https://en.wikipedia.org/wiki/Global_w arming
 Book- Environmental chemistry, By B.K. Sharma,
12th edition(2015), Page no.- 141 – 196.
 Book- Environmental chemistry, By A.K. De, 7th
edition (2010), Page no.- 32 – 41.
Greenhouse effect
Greenhouse effect

Greenhouse effect

  • 1.
    GUIDED BY- Dr. JAMESMATTHEW SUBMITTEDBY- NEHA MISHRA (M.Sc. 4TH sem.)
  • 2.
  • 3.
     Greenhouse abuilding made mainly of glass, with heat & humidity regulated for growing plants. The atmosphere acts like a glass in a greenhouse.  Atmosphere, like glass absorbs some of the long wave radiation emitted by earth and radiates the energy back to earth. In this way temperature of earth is maintained.  The atmosphere surrounding the earth in this manner plays a vital role in maintaining an even temperature on the earth’s surface.  A greenhouse is that body which allows the short wavelength incoming solar radiation to come in, but does not allow the long wave outgoing terrestrial infrared radiation to escape.
  • 4.
     Earth’s atmospherebottles up the energy of the sun, & is said to act like a greenhouse.  Carbon-dioxide present in the atmosphere acts like glass windows.  Carbon-dioxide and water vapours in the atmosphere transmit short wavelength solar radiation but reflect the longer wavelength heat radiation from warmed surface of the earth.  Carbon-dioxide molecules are transparent to sunlight but not but not to the heat radiation.  They trap the re-enforce the solar heat.  The Greenhouse effect defined as the progressive warming up of the earth’s surface due to blanketing effect of manmade CO2 in the atmosphere.
  • 8.
     The fourmajor greenhouse gases, which causes adverse effects are carbon-dioxide, methane, nitrous oxide and chlorofluorocarbon.  For the earth, water vapour is the most important of all greenhouse gases.  Water vapour absorbs IR in the region 2.5 to 3.5 µm 5 to 7 µm, as well as over a broad range above 13 µm. CARBON-DIOXIDE  It is a major contributor to greenhouse effect because it absorbs IR in the range of 14 to 19 µm, and completely blocks the radiation flux between 15 to 16 µm.  The burning of fossil fuels such as coal, tar, and natural gases release CO2 . Burning of wood, waste materials and tress release CO2.
  • 9.
    METHANE  Methane absorbradiation in the wavelength ranges from 3 to 4 µm and 7 – 8.4 µm (in the window region).  Methane gas increases stratospheric water vapour on oxidation and the rise in water vapour is more important source of greenhouse effect than the direct effect of methane gas. NITROUS OXIDE  Nitrous oxide absorb IR radiation in the ranges 3 to 5 µm and 7.5 to 9 µm (infrared window).  The major sources of nitrous oxide are microbial denitrification, conversion of nitrate to nitrous oxide soils, lake and oceans.  Methane gas is 24 times & nitrous oxide is around 320 times aggressive greenhouse gas than carbon dioxide.
  • 10.
    CHLOROFLUROCARBONS (CFCS)  CFCsabsorb in the range 8 to 12 µm with each CFC having specific absorption bands in the region.  CFCs are released into the atmosphere during the operations and maintenances of appliances and equipments using these molecules as coolants and propellants. HYDROCHLOROFLUROCARBONS (HCFCS)  The HCFCs also attenuate radiation within the same range, but their in the troposphere is much shorter than that of the CFCs.  The rate of increase of CFCs has declined by a factor greater than two in the past decade, but HCFC concentrations are increasing at a much higher rate.
  • 14.
    The greenhouse effectwill bring about the following important changes in the climate of the Earth.  As a result of rise in temperature of the earth due to greenhouse effect the oceans get warm up and sea level would rise flooding low lying regions.  In temperate regions, the winter will be shorter and warmer and the summer will be longer and hotter.  There will be enormous increase in rainfall but the problems of desertification, drought and soil erosion will further worsen.  The tropics may become wetter and the subtropics, which are already dry, are expected to be drier.  The plants & animals will also be affected resulting in the disruption of the whole ecosystem.
  • 16.
     Erik M.Conway(2008) defined global warming as “the increase in Earth’s average surface temperature due to rising levels of greenhouse gases”.  Global warming will lead to higher temperature and changes in rainfall, and this in turn will modify the extent and productivity of land suitable for agriculture. • For example, a temperature increase of 3ºC paired with a rainfall increase of 10% in the developing countries would cause a decrease of 11% productivity that could have serious consequences for food security.  According to latest climate change report, global warming would decrease crop production in developing countries but increase in industrialised world.  Global warming would also have short term and long term effects on human health and environment.
  • 18.
     The hotdays are sure to be scorching and cold ones freezing.  In future, the rain is going to be intensive.  Changes in frequency & intensity of extreme weather will have profound impact human society and natural resources.  A few study forecast an increase in the number of deep cyclones and increase in intensity of the storm over western Europe.  With the continuing increase in greenhouse gases in the 21st century, the losses caused by natural calamites and catastrophes are bound to increase.  A century from now, the Earth’s surface will be about 3.5ºC higher than in 1990.
  • 19.
     Surface oceanwaters today are roughly 30 percent more acidic than at the start of the Industrial Revolution.  In the last decade, the rate of Antarctica's ice mass depletion has tripled.  Scientists predict that the Arctic Ocean will barely have ice before 2050.  For the last twenty years, sea levels rose at twice their rate during the last century.  Global temperatures could increase by as much as 10.4 degrees Fahrenheit by 2100.
  • 22.
     https://www.britannica.com/science/global-warming  https://en.wikipedia.org/wiki/Global_warming  Book- Environmental chemistry, By B.K. Sharma, 12th edition(2015), Page no.- 141 – 196.  Book- Environmental chemistry, By A.K. De, 7th edition (2010), Page no.- 32 – 41.