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Resources/Materials
Needed:
Cellotape (Scotch tape); An old umbrella that you can cut up – or an
old piece of cloth; 12 plants (these can be grown from seed as a prior
activity); 2 liter flasks; Lemons; Water; Large glass jar or 5 pieces
of glass about 30 cm by 30 cm; 2 small vessels; Thermometer
(preferably alcohol, not mercury); Atlas or world map; Handout page
76.
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Target Age Group: 11-12
years
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Curriculum Areas: Science,
Geography, ICT, Art, Language
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Method Used: Experimentation,
Report Writing
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Safety: Make
sure that the umbrella or cloth is far away from the student underneath when the
other two students are cutting a hole in it. Be also very aware of the fragility
of the glass the students are using. Supervise the use of a mercury thermometer.
Climate
dictates much of the way the world is. All over the planet climate differs and
human activities, such as agriculture, have developed according to local
climatic conditions. Just as humans are influenced by the climate, they have
also influenced our global climate during the industrialized era. The increasing
number of people and economic development continue to cause adverse affects for
the global environment.
This activity will
allow students to understand key environmental issues and visualize the impact
human actions have on global atmospheric and water problems. The questions at
the end of this module will stimulate the students to think about the impact of
their daily activities on the environment.
Activities that
follow are chosen to explain three core concepts related to our atmospheric
environment: ozone depletion, acidification, and global warming. Although these
terms are frequently used, very often concepts like ozone depletion and global
warming are confused. All three environmental problems are linked to processes
in the atmosphere that are altered by the behavior of humans.
This
science project suggestion aims at explaining the different concepts to the
students. You may wish to begin, or conclude, this activity by reading the Climate
change and Ozone depletion sections of
Cawedu.net.
The
Ozone Layer is a layer in the upper atmosphere where a form of oxygen with three
atoms in a molecule (called ozone) is found. This layer protects us from harmful
ultraviolet (UV-B) radiation from the sun. In the seventies investigators
observed a “hole” in this layer at the poles. The cause of this hole turned
out to be the use of substances which destroy ozone (known as ozone depleting
substances), in particular the chlorofluorocarbons (CFCs). As a result of the
reduction of this layer the UV-B radiation that reaches the Earth increases.
This causes increased skin cancer risks and eye problems.
The depletion of
the ozone layer is a clear example that the environment does not have national
boundaries. CFCs were mainly used in industrialized areas, but its effect
concentrated at the polar areas. Table 1 shows the current ozone losses and
increase in UV-B as presented in the GEO2000 report (page 27).
Table
1 Current ozone losses and UV-B increases (GEO-2000)
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Ozone loss (%)
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UV-B increase (%)
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Northern hemisphere, mid-latitudes, winter/spring
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6
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7
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Northern hemisphere, mid-latitudes, summer/autumn
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3
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4
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Southern hemisphere, mid-latitudes, year-round
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5
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6
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Antarctic spring
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50
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130
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Arctic spring
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15
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22
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Note: Figure is approximate and
assumes other factors, such as cloud cover. Source in GEO-2000: WMO, NOAA, NASA
and EC (1998).
Sulphur dioxide
resulting from sulphur emission is washed out the atmosphere as acid rain. Acid
rain causes acidification. This is the process by which soil and water become
acidic.
The change of acid
levels in soils has a large impact on life in lakes and forests, but it also
causes crop losses. One of the main causes of sulphur emissions is the burning
of sulphur rich fuels, like coal. Although
strenuous efforts have begun to abate acid rains in many European and North
American countries, emissions in other regions, like Asia, are a major and
growing problem.
Climatology has a
big effect on acid rain. If prevalent winds of a region come from over the ocean,
unindustrialized or uninhabited area, the region is probably saved from acid
rain. On the other hand, even if the region itself uses the best available
technology and does not emit sulphur dioxide, it might still suffer from acid
rain due to winds coming from polluting areas.
Global
warming is the process whereby the average temperature of the atmosphere
increases due to the increase of so-called greenhouse gases in the atmosphere. A
greenhouse is a widely used metaphor for the warming function of the atmosphere.
Even though the effect is the same, the surface of the Earth below the
atmosphere and the space inside a greenhouse are warmer, the major mechanisms
functioning are different. In a greenhouse the roof and walls effectively
prevent convection
and advection and the heat is trapped within the greenhouse with the
air. In the atmosphere convection and advection redistribute the heat from
warmer to colder areas. The atmospheric greenhouse gases do not prevent
convection nor advection, they absorb terrestrial (infrared, long-wave)
radiation. Due to absorption they have a distinctive temperature which makes
them emit themselves long-wave radiation. The more greenhouse gases the more
absorption and emission. Part of this emission of long-wave radiation from
greenhouse gases is directed to the Earth's surface which heats up further. Read
more, and more!
One of the
greenhouse gases is carbon dioxide (CO2).
Mainly due to the burning of fossil fuels, the concentration of CO2
in our atmosphere has increased
significantly. However, the contributions of different parts of the
world differ considerably. Figure 1 shows CO2
emissions per capita expressed
in tonnes per year, for 1975 and 1995 (from the GEO-2000 report).

Note: Source in GEO-2000: CDIAC 1999
Global
warming is expected to have an impact on many things: melting of polar ice, an
increase of the sea level. Climate
patterns will change and this will also have an effect on the growth of plants,
the spreading of species and on the Earth’s ecosystems as a whole. Learn more
about climate change and the Caribbean in
the section Climate
change: impacts, adaptation and vulnerability of Cawedu.net.
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Bring an old - really old! - umbrella that can be cut up, or a piece of
cloth to the classroom.
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Ask one of your students to volunteer to sit underneath the umbrella on a
table at the front of the class.
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Then carefully, with a pair of scissors, get two other students to cut
holes in the umbrella.
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Shine a powerful torch or
spotlight (or sit outside in the direct sunlight) through the umbrella or piece
of cloth so that the children can see the dappled effect on the child sitting
underneath it.
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Ask one student to
explain what is UV and UV-B radiation, what are the effects of excess
exposure to UV-B radiation, what is the ozone layer and how it is connected to
the UV-B radiation:
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Apart from the warm
sunlight, other rays from the sun approach the Earth.
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One
type of radiation is ultraviolet or UV-B.
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This
causes skin problems (think of sunburn) and eye problems (eye cataracts).
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This
harmful radiation is kept away from the surface of the Earth by the ozone
layer.
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However,
apart from the tropics, this layer has become thinner, in most parts of the
world and especially in the polar areas, so the protection becomes less.
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Invite students to think
about what can be done about this problem: Apart from using sun cream, the
emission of the gases that damage the ozone layer should be stopped.
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Tell the students that
most governments have agreed to stop the production of CFCs that damage the
ozone layer.
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Tropics and sub-tropics have not been affected by the depletion of the ozone
layer. Ask the students
why it is still necessary that also the Caribbean countries need to take
measures to curb the ozone depletion: Ozone depleting substances used in
Caribbean mix throughout the atmosphere and cause depletion in vulnerable parts
of the world.
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Ask if the students know
in what products these gases are used?
Set up an experiment with two comparable
groups, each of six plants, group A and B: use the same soil for all plants, use
plants in similar health and of the same age and so on.
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Prepare two flasks of water: one with tap water and one with tap
water plus the juice of a squeezed lemon. Mark
the flasks respectively as A and B. Explain to the students that flask B will
simulate the acid rain.
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Water each group of plants
equally with their assigned flasks:
use flask A water for group A plants, and flask B water
for group B plants.
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Ask the students
to work in six groups and to continue the experiment for two weeks (or until
dramatic results in the degeneration in the health of group B plants are shown).
Each group is watering one pair of plants (A+B).
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Discuss the differences between the two groups of plants after two
weeks. Make an inventory of the differences observed and ask the students to
explain the differences.
Differences can be observed in freshness of leaves, colour of leaves, plant
growth etc.
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Explain to the students
that the outcome of their experiment is comparable with what has been observed
in forests that were damaged by acid rain.
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Use this as
an opportunity for the students to really apply the ‘scientific research
method’ to their investigations
in describing the experiment in a report. The students should include the
following: Introduction, Aim of the experiment, Hypothesis, Materials and
Methods used, Results and Conclusion.
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Discuss
weather acid rain is a problem of your particular country. Which factors are the
most dominant? Does climatology work in favor or against your country?
To
do a simple experiment to explain the working of a greenhouse:
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Get a large
glass jar or construct a glass box out of some panes of glass.
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Place a
small container of water under the glass and put another just outside of it.
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Leave both
in the sunlight and then, at the end of the day, take the temperature of the two
containers. Let the students find out which is warmer and why this is the case.
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Experience
drawn from the experiment or from people who have visited a green-house can be
applied to other examples of insulation such as clothes, sleeping bags, hot
water tank jackets etc, to illustrate heat retaining qualities and effects.
Explain that carbon dioxide gas does the same thing to heat within the
atmosphere (note the different mechanism though!!) and give examples based on the information above.
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The
consequences of the heating of the atmosphere can be discussed back in the
classroom, using a world map. Predict which areas and which people will be
affected most by the melting polar ice or alpine glaciers: sea level rise will
affect low lying areas – small islands might disappear, coastal areas are
threatened, etc. For more information about the effects of global warming see
the section Climate
change: impacts, adaptation and vulnerability of Cawedu.net.
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Instruct
the students to write up a full report including the following details (see
model for report):
All three of these experiments encourage
students to become more familiar with atmospheric changes and to be able to
differentiate between these three global problems. As a follow up, you may wish
to encourage your students to look further locally at how your region, or
country, is affected by these atmospheric changes. Allow them to explore the
local context in a homework or library assignment, and if these resources are
unavailable, they can use their imagination to write creatively about how their
home might be affected by these changes. The students can look for present or
predicted examples in their country of the impact of climate change (floods,
droughts, warmer seasons, hurricanes), ozone depletion (development of CFC
friendly products, increase in health risks, public awareness campaigns), acid
rain (forest degradation, water contamination, degradation of national
monuments). This will allow the students to bring these global issues down to
the local level.
A well designed
investigation and report.
(This science project suggestion has been adapted from
Pachamama Teacher's Guide, UNEP, ISBN: 92-807-2147-X)
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