UNIT 7: CLIMATE CHANGE
Key Unit competence
By the end of this unit, I should be able to discuss the climate change and
its impact on Rwanda and the other countries
Introductory activity1) Using internet research and other geographical materials make a
research to establish relationship between the following concepts:
i) Climate change and global warmingii) Green house phenomena and desertification
2) Basing on the knowledge acquired from the question 1, assess the
consequences of climate change on Rwanda.
3) Which area of Rwanda is likely to experience the desertification?
Give reasons supporting your answer.
7.1. Climate change: definition, causes and effects
Learning activity 7.1
Study carefully the below photographs and answer the questions
that follow:
1) What does climate change mean?
2) Explain how industries contribute to the climate change?
3) Describe the effects of climate change
7.1.1. Definition of climate changeClimate change refers to the long-term changes in average conditions and
characteristics of earth’s lower surface atmosphere resulting either from natural
variability or human activities that change atmospheric conditions of a region or
location. It is also defined as a long term change of climatic elements such as
temperature, rainfall, wind speed and direction, sunshine, atmospheric humidity,
atmospheric pressure, cloud cover over a given region of earth’s lower surface
atmosphere or globally.
7.1.2. Causes of climate change
The causes of climate change are classified into natural causes and man - made
causes
i) Natural causes of climate change
Natural causes of climate change include:
Variations in the earth’s orbital characteristics
The more elliptical orbit makes the earth to be once year in closest position to
the sun (Perihelion: 147 500 000 km) or in farthest position to the sun (Aphelion:
152 500 000 km). At the Aphelion, the earth receives the least solar energy
while the maximum is received at the Perihelion.
Volcanic eruptions
Volcanic activity affects the climate. World temperatures are lowered after a
series of volcanic eruptions. This is due to the increase in dust particles in the
lower atmosphere which will absorb and scatter more of the incoming radiation.
Sulphur dioxide gas is given off during some of the eruptions. This gas remains
in the atmosphere for as long as three years and it reacts with water vapor
and forms a bright layer in atmosphere. This layer reduces the amount of solar
radiation reaching the earth surface by reflecting some back to universe.
Variations in solar output
Sunspot activity which occurs in cycles, may significantly affect our climate.
Times of high annual temperatures on earth appear to correspond to periods
of maximum sunspot activity. The results found from satellites measurements
showed a decrease of 0.1% of the total solar energy coming to the earth in the
early 1980s. This value was obtained over a period of 18 months. It is predicted
that the increase in solar output of 1% per century will contribute to the increase
of the global average temperatures by between 0.50C and 10C.
Variation of aerosols in atmosphere
Aerosols like solid particles of varying sizes and liquid droplets which include:
ploughed soil cover, deserts, rocks, salt particles from seas and oceans;
meteoric particles, organic matter, such as bacteria, seeds, spores and pollen.
These particles help in selective scattering of shortwave electro-magnetic solar
radiation which adds varied color of red and orange at sunrise and sunset. Some
of the aerosols, mainly water droplets, absorb certain amount of solar radiation
while some amount of radiant solar energy is reflected back to the space. The
high concentrations of aerosols in atmosphere decrease the temperatures to
reach the earth surface.
Sunspots
Sunspots, defined as dark areas within photosphere of the sun and surrounded
by chromosphere, are created in the solar surface (photosphere) due to periodic
disturbances and explosions. These dark areas are cool areas because they are
characterized by 1, 5000C less temperature than remain part of photosphere.
The increase or decrease in number of sunspot is completed in a cycle of
11 years. It is believed that the energy radiated from the sun increases when
the number of sunspots increases and consequently the amount of insolation
received at the earth’s surface also increases.
ii) Human causes of climate change
Human activities have been the mostly responsible for atmospheric alterations.
Human activities participate highly in atmospheric pollution leading to the
change in composition of atmosphere.The atmosphere is polluted by human activities in the following ways:Variations of carbon dioxide in atmosphere
Carbon dioxide (CO2 ) is an important heat-trapping (greenhouse) gas. Itis released through human activities such as burning fossil fuels and gases
released from industries, as well as natural processes such as respiration and volcanic eruptions. There is a positive relationship between the concentration of
carbon dioxide in atmosphere and the global temperatures: high concentrations
of carbon dioxide result to the rise of temperature on the earth surface while low
concentrations of carbon dioxide result to the lower temperatures.
Forest and grassland fire
It increases the concentration of carbon dioxide in atmosphere resulting from
the burn of trees and grassland which are cut and put under fire for different
purposes.
Deforestation and land use changesWhen people clear large areas of forests and grasslands for cooking or
construction, they reduce the main disposal system for carbon dioxide from
atmosphere by photosynthesis, which leading to the increase of carbon dioxide,
and eventually to the increase of temperature on the earth surface.
Industrial developments
Gases like methane, nitrous oxide, chlorine, bromine and fluorine are added into
the atmosphere through industrial activities.
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.
UrbanizationThe buildings of cities increase the reflection and decrease the absorption of
solar radiation which would change the temperatures on the earth surfaces. The
urban activities participate also in increasing the concentrations of greenhouse
gases in atmosphere leading to the rise in temperature.
Increase in Population
It is obvious that this last two decades the people have been huge increase in
the population. Now, this has resulted in increased demand for food, cloth and
shelter. New manufacturing hubs have come up cities and towns that release
some harmful gases into the atmosphere which increases the greenhouse
effect. So, more people means more usage of fossil fuels which in turn has
aggravated the problem.
FarmingNitrous oxide is one the greenhouse gas that is used in fertilizer and contributes
to greenhouse effect which in turn leads to global warming.
7.1.3. Effects of climate change in the world (global, Africa, Rwanda)i) Effects of climate change in the world
The following are the effects of climate change in different parts of the world:
Increase in the amount of rainfall: A rise in global temperatures could leadto an increase of evapotranspiration. This could eventually lead to the rise in
amount of rainfall.
Melting of glaciers: A rise of temperature leads to the melting of glaciers inpolar and mountainous regions resulting into flooding. This would cause the
levels of the sea to rise by 20 cm by the year 2030.
Rise in the sea and ocean levels: The increase in the amount of rainfall andmelting of glaciers leads to the increase of the sea and ocean levels destroyingboth human and physical features at the coast.
Increases in intensity of extreme weather: Climate change increasesevents such as heat waves, tornadoes and hurricanes.The prolonged severe droughts: Some regions may experience prolongeddroughts caused by reduction in rainfall, which may result in aridity.Depletion of ozone layer: High amount of harmful ultraviolet radiationincreases the cases of animal and human diseases such as cancers, blindness
and other eye diseases.
Occurrence of acid rain: Acid rain is harmful to animal and human being.
Lower crop and timber yields: Since ultraviolet radiation slows down manyaspects of plant growth such as photosynthesis and germination in many plants
leading to low production.
Reduction of plankton growth: As temperature goes beyond coral reefsliving standard, fish breeding and feeding patterns are disrupted.
Decrease of agricultural production: In some regions, the rainfall maydecrease, or agriculture seasons be disrupted because of climate change.
Some regions became drier and make soil infertile for crop production.
City environments becoming warmer: The increase of carbon dioxidemakes the temperatures to increase most in urban areas.Water use and long-term planning: A wetter or drier climate can affectwater resources planning. Water reservoirs, dams, and hydroelectric projects
might become useless in coming years.
Spread of vector-borne diseases: Because of high temperature there canbe an increased range of insects.
Acidification of oceans: This can create a reduction in plankton, coral reefs
and a drop-in fishing yield.
ii) Effects of climate change in AfricaThe following are some of the facts showing the climate change and variability
in Africa:
– Melting of glaciers on the top of the highest African mountains such as
Kilimanjaro, Rwenzori, Kenya and Karisimbi;
– Warming in African tropical forests has been evaluated at 0.29 °C for
the past 10 years and 0.1 °C to 0.3 °C in South Africa, while it ranged
between 0.2 °C and 0.3 °C in the Nile Basin countries;
– Decreasing trends in temperatures; in eastern Africa, the situation has
been complex because they have been observed over the regions
close to the coast or major inland lakes and increasing in the rest of
the region;
– The gradual heating, between 1961 and 2000, over the continent
meant more warm spells (days) and fewer cold days across Africa.
An increase in temperature in Sahara desert has led to the decline in
volume of water in Lake Chad;
– Fluctuations of precipitation; the extent of variability is complicated and
exhibits more spatial and temporal fluctuations across the continent;
– The decrease in rainfall has been registered in West Africa (between 4 °
and 20 °North; 20 °West and 40 °East), by up to 20% to 40% for the
periods 1931-1960 and 1968-1990 respectively. A similar decline in
mean annual rainfall has also been observed in the tropical rain-forest
zone. A reduction of around 4% in West Africa, 3% in North Congo
and 2% in South Congo for the period 1960-1998.;
– Increases in rainfall have been registered in different parts of southern
Africa (e.g., Angola, Namibia, Mozambique, Malawi, and Zambia);
– Increase in the desertification in south of the Sahara desert;
– Links have also been identified between the warm Mediterranean Sea
and abundant rain fall over the surrounding regions.
iii) Effects of climate change in Rwanda
Rwanda experiences some rainfall events that cause unexpected flooding and
catastrophic events such as landslides etc. These extreme events are attributed
to climate change. The figure below represents some effects of extreme rainfall
events of climate change in Rwanda.
The following are effects of climate change in Rwanda:
– Significant increase in precipitations at a rate of between 2 and 6.5 mm
per year over the Congo-Nile crest and the northern highlands for the
period of 1935–1992.
– Floods that occurred in May 2002 caused the death of 108 persons in
North western regions while the one occurred in 2007 have resulted to
displacement of more than 456 families and destruction of hundreds of
hectares of crops in Bigogwe sector in Nyabihu District;
– During September 2008 heavy rainfall accompanied by winds affected
8 of the 12 sectors of Rubavu district and provoked the displacement
of more than 500 families, caused the destruction of about 2,000
hectares of crops and many other infrastructures;
– Floods reported in September 2012 in Nyabihu, Rubavu, Bugesera
and Kirehe districts whereby more than 1000 families were displaced
and their crops submerged completely;
– The landslides and floods caused by heavy rainfall are regulary observed
mainly in north- western parts of Rwanda (Rulindo, Gakenke, Musanze,
Nyabihu and Rubavu districts). For instance, the floods which occurred
on 2nd and 3rd April, 2016 caused the death of 12 people, with 19
injured and destruction of 196 houses across the country. The floods
which took place in Musanze district on 20th April 2016 caused the
destruction of 64 houses and many hectares of crops and cattle;
– The significant increase in mean annual temperatures of between 0.036
and 0.066 °C per year for the period of 1961-1991;
– Since 1902, a number of famines following prolonged droughts
episodes have been registered in Rwanda notably in eastern and
south-eastern regions;
– More occurrences of lightning combined with the thunderstorms in
2013 caused 12 deaths in Karongi, 12 in Rubavu, 4 in Rusizi and 5
death in Rutsiro districts, respectively. The same districts suffered from
the same extreme weather events which were reported to cause 15
deaths in 2015 (January-October) with 30 people injured.
Application activity 7.1
1) Identify the areas of Africa that are susceptible to face the climate
change challenges?
2) Describe the effects of climate change in Eastern and Western
provinces of Rwanda.
7.2. Global warming and the green house phenomena(definition, causes and the effects)
Learning activity 7.2
1) Use different resources to find the meaning of the following:
i) Global warmingii) Green house phenomena
2) Explain the reasons of practicing greenhouse farming.
7.2.1. Definitions of global warming and greenhousephenomena
These two phenomena of global warming and greenhouse are related but are
different.
i) Global warming
Global warming refers to the gradual rise in world temperatures. This is a gradual
increase in the average temperature of the earth›s atmosphere and oceans due
to increase in the amount of carbon dioxide. The increase in the amount of
carbon dioxide leads to greenhouse effect. It is a change that is believed to be
permanently changing the earth›s climate. An increase in greenhouse gases
increases the greenhouse effect which in turn increases the global warming.
In the last 100 years, the mean surface temperature on earth has increased by
0.5 °C.
i) Greenhouse effect
The greenhouse effect is a phenomenon in which the atmosphere of a planet
traps radiation emitted by sun. It is caused by gases such as carbon dioxide,
water vapor, and methane that allow incoming solar radiation to pass through
but retain heat radiated back from the planet’s surface.
7.2.2. Causes of global warming and green housephenomena
The following are the causes of global warming and green house phenomena:
1) Human factorsHuman activities produce various gases ejected in the atmosphere that are
responsible for the global warming. These activities are destroying earth at fast
rate: the emission of carbon dioxide from industries and vehicles, the burning
of fossil fuels, cutting of trees and forests to build some new buildings and new
malls, dumping of trash everywhere and not even recycling it, excessive use of
the plastics and smoke from factories. All the activities performed by human
beings are the major factors for gases that pollute the air and warm up the earth.
These may contribute to the destruction of the ecological balance of the nature
leading to the global warming.
Burning of fossil fuels
Fossil fuels are burnt on day-to-day basis. This activity produces large
percentage of gases such as carbon, petroleum, coal and many other different
gases which are emitted in earth’s atmosphere. Carbon dioxide being one of
gases with greenhouse effect is provided in excess in our atmosphere in far
greater quantity in comparison with other gases produced by human activities.
Use of chemical fertilizersThe use of the artificial chemicals for crops has become one reason for the global
warming. These chemicals are dangerous to the earth as well as to the human
beings. These fertilizers are rich in the nitrogen oxide which is more dangerous
than the carbon dioxide. Those oxides of nitrogen destroy ozone layer even
faster than other greenhouse gas and hence let harmful ultraviolet rays enter
atmosphere thus making earth warm and leading to the global warming.
Industrial advancement
More and more different industries and factories are set up in modern world to
meet needs of the human beings. These factories need large amount of fuels like
some coal, petroleum for power generation and electricity required by machines
to work. Burning of these fuels also releases large amount of the carbon dioxide
which absorbs harmful radiations from sun making it warm, hence increasing
global warming.
Deforestation
The mass removal of trees, called deforestation, also affects the amount of
carbon dioxide in our atmosphere. Forests around the world are being cleared
for cultivation, mining, building, roads building, grazing cattle, etc. As they grow,
trees take in carbon dioxide. When trees are removed, the carbon dioxide that
they could have removed from the atmosphere is left. Cut-down trees are often
burned. Burning produces more carbon dioxide. If the trees are cut, plants will
not be able to produce oxygen and concentration of the carbon dioxide will
increase. Increase of the carbon dioxide in air is very harmful for the human beings
and also disturbs water cycle and hence total imbalance of our ecosystem. So
being one of greenhouse gases it will lead to the global warming.
Air pollutionThe harmful gases emitted from vehicles and the factories and greenhouse gases
cause some pollution in the air and these gases get captured in atmosphere.
The smoke gather up in atmosphere forming some clouds full of harmful gases
which later fall as the acid rain which destroys plants. Plants provide us with
oxygen and if they die level of carbon dioxide will increase in atmosphere which
is known as a harmful gas. These gases emit heat which increases temperature
of earth, hence causing global warming.
2) Physical factorsVolcanic eruptions
Volcanic eruptions are also among the causes of global warming. These eruptions
contain the dust particles and gases like the sulfur dioxide which stays in the
atmosphere for years and blocks the sunlight from reaching surface of earth
making it somewhat cool. These dust particles affect balance of atmosphere
and become contributing factor of the global warming.
Depletion of ozone layer
Depletion of ozone layers is an important factor that causes global warming.
The ozone layer is known as the layer outside the atmosphere which protects
surface of the earth from harmful ultra-violet and the infrared radiations causing
some dangerous diseases like the skin cancer. Ozone layer depletion is one
of causes of the global warming; entering of the harmful gases which helps
in heating up the earth but other greenhouse gases like the carbon dioxide
and methane that helps in heating up and tears up ozone layer making a hole
called “Ozone hole”. So, ozone layer depletes due to these gases which allowultra violet radiations to enter the earth’s atmosphere making it more warm than
normal and also affects temperature leading to the global warming.
7.2.3. Impact of greenhouse process on global warming
Greenhouse effect is a process in which the atmosphere of the earth traps
some of the heat coming from the sun and fails to radiate, making earth warming.
This is due to the burning fuels, cutting of trees, concentration of the heat on
earth is increased to some abnormal levels making the greenhouse effect as
one of the major causes of the global warming. Carbon dioxide, nitrous oxide
and methane are the greenhouse gases which help to keep earth warm. It is
natural phenomenon that takes place with adequate concentrations of some
greenhouse gases. When concentration of these gases rises then they disturb
climatic conditions, thus making earth warmer. These gases are not able to
escape and that causes the worldwide increase in temperatures. So balance of
the carbon dioxide and some other gases should be maintained so that it does
not become major reason for the global warming.
Application activity 7.21) Explain why causes of climate change and green house differ in rural
and urban areas.
2) Among the effects of climate mentioned above, which ones do you
observe in your local environment?
3) Referring to the greenhouse phenomenon, describe the advantages
and disadvantages of the farming practiced in greenhouse.
7.3. Adaptation measures and mitigation for the climate changeLearning activity 7.3
In your local environment, identify any evidence of climate change and
propose sustainable strategies to deal with it.
7.3.1. Adaptation measures for climate changeAdaptation for climate change refers to measures and strategies taken to
cope with climate change and variability. These measures vary from one domain
to the other like agriculture, livestock keeping, tourism, public health and
water management; from one climatic region to the other as dry, wet, hilly, flat,
depression, mountains, floodplains; from season to season as in dry and wet
seasons; and across diverse actors as private, public, national, international,
NGOs, local communities. Hence, adaptation measures are many and are not
homogeneous. Some of them are briefly described below:
Maintaining current ecosystems wherever possible: This impliesstrengthening, extending and in some cases refining global protected area
networks to focus on maintaining large blocks of intact habitat with a particular
emphasis on climate change.
Agro-forestry: This is a land-use system that incorporates trees in food cropfields. In other words, it is a combination of agriculture and forestry for more
diverse, profitable, productive and sustainable land use.
Progressive and radical terracing: This is used to reduce runoff, soilerosion and landslides. At the same time, terracing helps to improve soil
quality and moisture retention, especially in steep areas.
Soil fertility conservation: Practices like the use of manure, mulching,planting of leguminous crops help to improve soil fertility by increasing the
micro-organism composition in the soil.
Seed and grain storage: This involves collecting seeds and grains fromfarmers at post-harvesting season and releasing them within the timely agreed
periods.
The use of pesticides: It is a wide range use of compounds such asinsecticides, fungicides, herbicides, rodenticides, molluscicides, nematicides,
plant growth regulators and others to control pests, insects, fungi, weeds,
bacteria, rodents, all of which are harmful to crops.
Ecological pest management: This is the use of natural enemy dynamicsor environmental positioning (e.g. crop shading) to eliminate or reduce the
presence of pests.
The use of improved seeds and species: This is vital to improve cropproductivity.Crop varieties and diversification: This measure consists of integration ofdifferent varieties of crops and hybrids of a particular crop. Multiple cropping
aids in replenishing the soil and maintaining its fertility by ensuring that there
is a constant balance of nutrients by decreasing dependence and saturation
of any one product.
Land use consolidation programmes: This encourage farmers withadjacent lands to grow the same crop. This facilitates the provision of inputs
(e.g. seeds and fertilizers), post-harvest activities (e.g. driers, seed and grain
storage facilities) and safer and faster transport of agricultural products.
Rain water harvesting: It is the practice of collecting and storing rainwaterfrom rooftops, land surfaces or rock catchment areas for different use.Irrigation like drip irrigation is a practice based on the constant applicationof specific and controlled quantity of water to the crops. The system uses
pipes, valves and small drippers or emitters that transport water from the
sources (i.e. wells, tanks and reservoirs) to the root area and applying it in
controlled quantities and pressure specifications while Sprinkler irrigationinvolves spraying the crops with water using sprinklers in a manner that
resembles rainfall.
Wastewater use: It forms a reliable source for crop irrigation and a positiveway to dispose of sewage water. Whereas wastewater contains a lot of
nutrients on the one hand, it carries pollutants like micro and macro organic
and inorganic matters that potentially pose hazards to human health, the
environment, crops and soils, on the other.
Biotechnology of crops: It involves the practical application of biologicalorganisms, or their sub-cellular components in agriculture and livestock. The
techniques currently in use include tissue culture, conventional breeding,
molecular marker-assisted breeding and genetic engineering.
Barrier crops: These are crops that are used as a cultural control strategyfor reducing the spread of pests and diseases to the most vulnerable crops.
These crops provide benefits over “hard infrastructure” in a number of ways:
first, they offer a natural form of protection; second, they contribute to the
biodiversity and often soil improvement; third, they can provide an added
source of food provisions or income and, finally; they can play a determinant
role in soil erosion reduction.
Integration of meteorological information in agriculture: It is used todevelop early warning systems, crop monitoring and disaster management.Training farmers: By offering short courses, seminars and group discussionson the impacts of climate changes and on various ways of adaptation.Facilitating the farmers: this consists of facilitating farmers to accesscapital that they need to purchase seeds, installation of tube wells, drilling
of pumping sets, chemical fertilizers, plant protection chemicals, tractors,
harvesters, threshers and other accessories.
Development of infrastructure: This concerns the improvement oftransport networks, electricity and marketing facilities which use to be
affected by climate change phenomena to promote a sustainable livelihood
of population.
Development of agricultural institutions: The institutions such asuniversities provide experts and researchers who offer critical services
like assessment, promotion of agricultural and livestock innovations and
dissemination of research findings to agronomists and farmers at all levels.
7.3.2. Measures for mitigating the climate change
Mitigation measures for climate change consist of actions to limit the magnitude
and the rate of long-term climate change. Climate change mitigation generally
involves reductions in human (anthropogenic) emissions of greenhouse gases.
Anthropogenic greenhouse gases include carbon dioxide (CO2), methane(CH4), Nitrous oxide (N2O) and a group of gases referred to as halocarbons.The following are mitigation measures for climate change:
Storing and reducing carbon dioxide: Carbon dioxide can be captured and
stored, but also it can be reduced. Carbon dioxide Capture and Storage (CCS)
is a process consisting of the separation of CO2 from industrial and energy
related sources, transport to a storage location and long-term isolation from the
atmosphere. Conserving electricity is one strategy to reduce CO2.
When we conserve electricity, we reduce the amount of fossil fuel that must be burnt. One
way to save fuel is to change daily activities that rely on energy from burning
fuel.
Use of energy that reduces the atmospheric pollution: The use of
renewable energy supply technologies, particularly solar, wind, geothermal and
biomass are recommended to reduce the atmospheric pollution. Renewable
energy systems such as hydro-electricity can contribute as well to the security
of energy supply and protection of the environment.
Reduction of the energy use in buildings: Cooling energy use in buildings
can be reduced by different measures, for example reducing the cooling load by
building shape and orientation.
Land-use management: Forest land, cropland, grassland, wetlands,
settlements have to be well managed by fighting against any threaten to them.
Changes in land use may result in net changes in carbon stocks and in different
impacts on water resources.
Crop land management: The use of agricultural practices which promote
the conservation of water, and its quality. There is a need for improved crop
and grazing land management to increase soil carbon storage; restoration of
cultivated peaty soils and degraded lands.
Afforestation and reforestation: The increase of number of trees helps to
capture the CO2 and decreases the flow of water from catchments.
Solid waste management and waste water treatment: Controlled landfill
(with or without gas recovery and utilization) controls and reduces greenhouse
gas (GHG) emissions but may have negative impacts on water quality in the
case of improperly managed sites.
Application activity 7.3
1) If you were the Director General of REMA, demonstrate the adaption
measures to climate change in Rwanda.
2) Suppose that you are a manager of a big industrial complex, describe
the strategies to mitigate climate change.
3) Explain the process by which the use of refrigerator contributes to
climate change.
7.4. Desertification (definition, causes, effects)
Learning activity 7.4
Study the photograph below and answer the questions that follow:
1. Explain what happen in the area shown in the photograph.
2. Explain how climate change contributes to desertification.
3. Referring to the figure below, describe the challenges that face
people living in desert areas.
7.4.1. Definition of desertification
Generally, desertification is described as the turning of the land into desert. It
is the process by which the land undergoes degradation from which a relatively
dry land region becomes increasingly arid, typically losing its bodies of water as
well as vegetation and wildlife. Desertification is caused by a variety of physical
factors, mainly the climate change and human activities.
7.4.2. Causes of desertification
Desertification is caused by a combination of factors that change over
time and vary with location. These include the following:
Less rainfall (total amount) and increased drought (frequency and
intensity) lead to drought of rivers and water bodies and decrease in protective
vegetation cover.
Global warming: It causes higher temperatures and increased
evapotranspiration. This reduces condensation and leads to shortage of
rainfall.
Population growth: The effect of this is the over-cultivation which reduces
soil fertility and leaves the soil exposed to erosion.
Deforestation: An increased demand for cultivation land, wood for cooking,
heating, building, increases the risk of soil erosion.
Poor crop cultivation practices: Some farmers do not know how to use
the land efficiently. Farmers may essentially strip the land of everything that
it has before moving on to another plot of land. By stripping the soil of its
nutrients, desertification becomes more and more of a reality for the area that
is being used for farming.
Urbanization and other types of land development: Development can
cause people to go through and kill the plant life. It can also cause issues
with the soil due to chemicals and other things that may harm the ground. As
areas become more urbanized, there are less places for plants to grow. This
can contribute to the process of desertification.
Soil erosion: The losses of the top soils and vegetation leads to the
desertification.
Climate Change: Climate change plays an important role in desertification.
As the days get warmer and periods of drought become more frequent,
desertification becomes more and more eminent. Unless climate change is
slowed down, huge areas of land will become desert; some of those areas
may even become uninhabitable as time goes on.
Over exploitation of the land of resources: If an area of land has natural
resources like, oil, or minerals, people will come in and mine it or take it
out. The removal of resources is usually associated with the striping of the
soil and depletion of nutrients. Consequently, plants are died and from therestarts the process toward becoming a desert biome as time goes on.
Natural disasters: There are some cases where the land gets damaged
because of natural disasters, such as natural fires, drought, floods, andearthquakes.
Rise of salinity: In the soil which causes the vegetation to be stunted.
Overgrazing: If there are too many animals that are overgrazing in certain
spots, it is difficult for the plants to grow back. Biomes are affected and losetheir original vegetation.
7.4.3. Effects of desertification
The following are the major effects of desertification:
Farming becomes unproductive: If an area becomes a desert, it’s almost
impossible to grow substantial crops there without special technologies.
This can cost a lot of money to try and do so as many farmers will have to sell
their land and leave the desert areas.
Hunger (famine): Without farms in these areas, the food that those farms
produce will become much scarcer. The people who live in those local areas
will be a lot more likely to try and deal with hunger problems. Animals will also
go hungry due to food shortage.
Flooding: Without the plant life in an area, flooding is much more eminent.
Some huge rivers cross deserts which experience a lot of flooding because
there is nothing to stop the water from gathering and going all over the place.
Poor water quality: If an area becomes a desert, the water quality is going
to become a lot worse than it would have been otherwise. This is because
the plant life plays a significant role in keeping the water clean and clear.
Overpopulation of the new areas: When areas start to become desert,
animals and people will go to other areas where they can actually thrive. This
causes overcrowding and overpopulation, which will, in the long run, end up
continuing the cycle of desertification that started this whole thing anyway.
Poverty: All of the issues that are described above (related to the problems
of desertification) can lead to poverty if it is not kept in control. Without food
and water, it becomes harder for people to thrive, and they take a lot of time
to try and get the things that they need for their subsistence.
Acceleration of desertification: The increased frequency and severity of
droughts resulting from projected climate change is likely to further accelerate
desertification.
Involuntary migration: Rural population affected by the effects of climate
change, especially the drought or aridity migrate towards different areas. This
may also lead to rural exodus.
Shortage of drinking water and water to use for other purposes:
This is where overpopulation causes pressure to exploit dry lands for farming.
These marginally productive regions are overgrazed, the land is exhausted,
and groundwater is over drafted.
Application activity 7.4Observe carefully the picture below and answer the questions that follow:
i) Referring to the factors of desertification discussed above, describe
the causes of the above phenomenon.
ii) Explain the effects of drought to the people living in such area.
iii) Considering the physical conditions of Rwanda, suggest the districts
in which the above phenomenon is likely to happen and the strategiesto limit this problem.
Skills Lab
Provide specific examples and analyze how human activities affect climate change.
End unit assessment
1. Compare the factors that can cause the climate change in China
and Rwanda.
2. Explain the causes of climate change in developed and developing
countries.
3. The World needs to develop at high rate with its industrialization
processes which is among the most causes of greenhouse effects.
Suggest the mitigation measures for climate change in this regard.
4. The world is facing the problem of climate change and this is
substantially leading to the problem of desertification.
a. Indicate the most affected areas by that problem?
b. Suggest the sustainable strategies to address the problem ofdesertification.