ESD02. Global Env.tal Problems-1
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Transcript of ESD02. Global Env.tal Problems-1
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GLOBAL ENVIRONMENTAL PROBLEMSPart-1
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Global Environmental Problems
Occurrence of these problems may be local in nature, but its effects /impacts / damages may not be limited to local or regional level; but these
are recorded across the globe. e.g.
Global warming,
Acid rain marine pollution
Trans-boundary movement of hazardous waste, etc.
The occurrence of these problems is not local in nature. These problems
may occur throughout the globe in various countries.
e.g. deforestation, desertification, etc.
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Types of Global Environmental Problems
Global Warming
Ozone layer depletion
Acid Rains or Acid Deposition
Loss of bio-diversity
Trans-boundary movement of hazardous wastes and chemicals
Deforestation
Desertification
Marine pollution
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Issues – Global Environmental Problems
Have long-term effects on people or societies:
Are either impossible or difficult to remove / reverse in short time duration
May require international efforts for solution
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Global Warming
Green House Gases
Responsible for
Green House Effect
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Total Co2 Emssions by country
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Enhanced Green House Effect
Various Green House Gases in
Atmosphere
Human Activities – release CO2 &other air pollution
Collection in the atmosphere
Acts like a thick blanket
Traps the Sun’s heat
Ultimately, Planet warms up
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Phenomenon
Global Warming - Increase in Earth’s average temperature (Atmosphere &
Oceans)
According to certain observations in the last century, Global surface
temperature has risen by
• 0.6°C (plus or minus 0.2°C) since the late-19th century, and
• about 0.4°F (0.2 to 0.3°C) over the past 25 years*
It is not a uniform phenomenon and has considerable uncertainty
Regarding
Extent of temperature rise,
Scale,
Timing,
Regional distribution, etc.
Note: * - Source: http://lwf.ncdc.noaa.gov/oa/climate/globalwarming.html
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Gases responsible for Global Warming
Green House Gases (GHGs):
Carbon Dioxide
Methane
Nitrous Oxide
Choro-fluoro-carbons
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GLOBAL WARMING – Consequences
Rising temperature of atmosphere and earth’s surface
Melting of ice in the polar regions
Rise in sea levels causing coastal flooding
Change in regional climate
Alter forests, crop yields and water supplies
Ecosystem
Human health
Expansion of deserts into rangelands, forest areas, agricultural areas
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Illustrations showing signs of Global Warming
Garhwal Himalayas, India
Glacial retreat at record pace. The Dokriani
Barnak Glacier retreated 66 ft (20.1 m) in
1998 despite a severe winter. The Gangorti
Glacier is retreating 98 ft (29.9 m) per year.
At this rate scientists predict the loss of allcentral and eastern Himalayan glaciers by
2035. (Reference: 1998. Himalayan glacier
backing off. Science 281:1277).
Source: http://earthobservatory.nasa.gov/Newsroom/NasaNews/2002/200205299370.html
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Ozone Layer Depletion
Ozone – one of the most important
constituents of the atmosphere Form of
Oxygen
Ozone shield:
Stratosphere
It absorbs the harmful ultra violet (UV)
radiation from the sun
Ozone layer is critical for the survival of
most life present on the Earth
Source: www.ns.ec.gc.ca/udo/ozone.html
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Destruction of Catalytic Ozone:
O3 + X → XO + O2
XO + O3 → X + 2O2
2O3 → 2O2
‘X’ chemical triggers ‘Chain Reaction’
Estimated says that single chlorine atom can destroy, more than
100,000 Ozone molecules before it is eliminated by other
reactions.
Ozone Layer Depletion
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Catalyst responsible for Ozone layer depletion
Important catalysts in Stratosphere:
Nitric Oxide (NO), hydroxyl (OH), Chlorine (Cl2), Bromine (Br)
XO –NO2, H2O, ClO and BrO
Sources of catalytic agents:
Natural phenomenon & Human activities
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Ozone Layer Depletion – Causes
Due to human activities:
1960s: Supersonic transport airplane (nitrogen oxides–
Harold Johnston)
1970s: Space shuttles (chlorine)
1974: Aerosol spray cans (CFCs – Molina and Rowland)
Nuclear test explosions & Bromine bombs Currently: Supersonic aircraft ‘High Speed Civil Transport’
Natural factors:
Supernova (stellar explosion)
Meteors and asteroids
Solar flares emit energetic particles that peirce the upper
layers of the ozonosphere
Its impact is very
small and hencethreat to life is also
less.
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Characteristics of Catalytic agents
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Consequences or Effects
Affects heat balance on the earth, which may lead to modification ofclimate.
Increases the UV radiation on the surface of the earth affecting the
organisms adversely: sunburns, snow-blindness, eye damage, cataracts,
ageing, wrinkling of skin, damage to immune system and skin cancer.
Affects several plants species – slow down of photosynthesis, delaying
germination, reduction in leaf size, stunted growth, poor seed quality,
increased susceptibility to weeds, pests etc.
Can depress photosynthesis in marine algae and can kill several species.
As it can penetrate 10 to 20m deep in water, can upset marine ecology
and lower fish yield.
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Illustration showing signs of Ozone layer Depletion
Ozone Hole over Antarctica:
These images from the Total Ozone
Mapping Spectrometer (TOMS) show
the progressive depletion of ozone
over Antarctica from 1979 to 1999.
This "ozone hole" area:
September 1996 - 10.0 million square
miles
September 1998 - 10.5 million square
miles
It develops each year between late
August and early October.
Regions with higher levels of ozone are
shown in red
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