CLIMATE CHANGE : Detailed Notes & Exam Questions | Grade 12 Geography Unit 2

CLIMATE CHANGE : Detailed Notes & Exam Questions | Grade 12 Geography Unit 2

Hello dear student! Welcome to Unit 2. In this unit, we will study one of the most important issues facing our world today — Climate Change. You have probably heard about it on the news, but do you really understand what it means, what causes it, and how it affects Ethiopia and the world? By the end of this lesson, you will be able to answer all these questions confidently. Let us begin step by step!

2.1 Basic Concepts of Climate Change

Before we talk about climate change, we need to understand some basic concepts clearly. Many students confuse weather and climate. Can you tell the difference? Let us find out!

Weather vs. Climate

Weather refers to the short-term conditions of the atmosphere at a specific place and time. It includes temperature, rainfall, wind, humidity, and atmospheric pressure measured over a short period — such as a day, a week, or even a month. For example, saying “Today is rainy and 22°C in Addis Ababa” is describing weather.

Climate refers to the long-term average of weather conditions over a long period — usually 30 years or more. For example, saying “Addis Ababa has a mild climate with an average annual rainfall of about 1,200 mm” is describing climate.

Key Point: Weather is what you get (short-term); Climate is what you expect (long-term). Climate is the average pattern of weather over a long period.

What Is Climate Change?

Climate change refers to significant and lasting changes in the statistical distribution of weather patterns over periods ranging from decades to millions of years. It includes changes in average weather conditions, as well as changes in the frequency and intensity of extreme weather events.

In modern usage, “climate change” usually refers specifically to the changes observed since the mid-20th century and the changes expected in the future, which are largely attributed to human activities — particularly the burning of fossil fuels.

Global Warming vs. Climate Change

Are these two terms the same? Not exactly!

Global warming refers specifically to the increase in the Earth’s average surface temperature. It is just one aspect of climate change.

Climate change is a broader term that includes global warming AND all the other changes that result from it — such as changes in rainfall patterns, rising sea levels, more frequent extreme weather events, shifts in ecosystems, and more.

Exam Note: Global warming is a subset of climate change. All global warming is part of climate change, but not all climate change is just warming — it also includes changes in precipitation, wind patterns, and extreme events.

The Greenhouse Effect

Now, here is a very important concept. Have you ever been inside a greenhouse used for growing plants? It gets warm inside even when it is cold outside, right? Something similar happens to our Earth!

The greenhouse effect is a natural process where certain gases in the Earth’s atmosphere trap heat energy from the Sun, keeping the Earth warm enough to support life. Without the natural greenhouse effect, the Earth’s average temperature would be about $-18°C$ instead of the current average of about $+15°C$.

Here is how it works, step by step:

  1. Solar radiation (shortwave) passes through the atmosphere and reaches the Earth’s surface.
  2. The Earth’s surface absorbs this energy and warms up.
  3. The warmed Earth then radiates heat back as infrared radiation (longwave).
  4. Greenhouse gases in the atmosphere absorb some of this infrared radiation and re-radiate it in all directions, including back toward the Earth’s surface.
  5. This trapped heat keeps the atmosphere warm — like a blanket around the Earth.
SUN ↓↓↓ (shortwave solar radiation) ┌───────────────────────────────┐ │ ATMOSPHERE │ │ │ │ Greenhouse gases trap heat │ │ ↑↓ ↑↓ │ └───────────────────────────────┘ ↓↓↓ (re-radiated infrared heat) ══════════════════════════════════ EARTH SURFACE (absorbs & warms)

Greenhouse Gases (GHGs)

The main greenhouse gases in the atmosphere are:

Greenhouse GasChemical FormulaSourceContribution to Warming
Carbon Dioxide$\text{CO}_2$Burning fossil fuels, deforestationLargest contributor (~76%)
Methane$\text{CH}_4$Agriculture, livestock, landfillsSecond largest (~16%)
Nitrous Oxide$\text{N}_2\text{O}$Fertilizers, industrial processes~6%
Chlorofluorocarbons (CFCs)VariousRefrigerants, aerosolsSmall but potent
Water Vapor$\text{H}_2\text{O}$Evaporation (natural)Most abundant GHG

Think about this: Water vapor is actually the most abundant greenhouse gas, but human activities do not directly control its amount. The gases that humans are increasing significantly are carbon dioxide, methane, and nitrous oxide.

Key Point: The greenhouse effect is NATURAL and necessary for life on Earth. The problem is the ENHANCED greenhouse effect — human activities have increased the concentration of greenhouse gases beyond natural levels, trapping MORE heat and causing global warming.
Exam Note: Remember: $\text{CO}_2$ is the biggest contributor to the enhanced greenhouse effect from human activities. Methane ($\text{CH}_4$) is about 25 times more potent than $\text{CO}_2$ at trapping heat over a 100-year period, even though there is less of it in the atmosphere. Nitrous oxide ($\text{N}_2\text{O}$) is about 300 times more potent than $\text{CO}_2$.

Practice Questions — Basic Concepts

Q1. Differentiate between weather and climate. Give one example of each from your local area.

Answer:
Weather: The short-term atmospheric conditions at a specific place and time. Example: “It rained heavily in Hawassa this morning with thunder and lightning.”
Climate: The long-term average of weather conditions over 30 or more years. Example: “Hawassa has a tropical climate with an average annual temperature of about 20°C and annual rainfall of about 1,000 mm.”

Key difference: Weather changes daily; climate is the long-term pattern.

Q2. Why is the greenhouse effect considered both a natural and a human-caused process?

Answer:
Natural greenhouse effect: Certain gases in the atmosphere (water vapor, $\text{CO}_2$, methane) naturally trap some heat from the Sun, keeping the Earth’s average temperature at about $+15°C$ instead of $-18°C$. Without this, life as we know it would not exist.
Enhanced (human-caused) greenhouse effect: Human activities — especially burning fossil fuels (coal, oil, natural gas), deforestation, agriculture, and industrial processes — have significantly INCREASED the concentration of greenhouse gases beyond their natural levels. This traps MORE heat than the natural process would, causing the Earth to warm beyond its natural temperature range.

So the mechanism is natural, but humans have made it much stronger.

Q3. List the four main anthropogenic (human-caused) greenhouse gases and state the largest contributor.

Answer: The four main anthropogenic greenhouse gases are:
1. Carbon dioxide ($\text{CO}_2$) — the LARGEST contributor (~76% of anthropogenic warming)
2. Methane ($\text{CH}_4$) — second largest (~16%)
3. Nitrous oxide ($\text{N}_2\text{O}$) — ~6%
4. Chlorofluorocarbons (CFCs) — small but very potent

Carbon dioxide from burning fossil fuels is by far the largest contributor to the enhanced greenhouse effect.

2.2 Trends in Global Climate Change

Now that we understand what climate change is, let us look at the actual evidence. Is the Earth really getting warmer? What do the numbers tell us?

Rising Global Temperatures

Yes, the Earth is definitely getting warmer. Scientific records show that the Earth’s average surface temperature has increased by about $1.1°C$ since the pre-industrial era (1850–1900). Most of this warming has occurred in the past 40 years, and the past 10 years have been the warmest on record.

$$\Delta T \approx 1.1°C \text{ (increase since pre-industrial era)}$$

This may sound like a small number, but remember — this is the AVERAGE over the entire planet. Some regions are warming much faster. And even a $1.1°C$ increase in global average temperature represents an enormous amount of additional heat energy trapped in the Earth’s system.

Rising Atmospheric CO₂ Concentration

Before the Industrial Revolution, the concentration of $\text{CO}_2$ in the atmosphere was about 280 parts per million (ppm). By 2023, it had risen to over 420 ppm — an increase of about 50%!

$$\text{Increase in CO}_2 = \frac{420 – 280}{280} \times 100\% \approx 50\%$$
Key Point: The current $\text{CO}_2$ concentration of over 420 ppm is the HIGHEST it has been in at least 800,000 years (and likely much longer). This is directly linked to human activities, especially the burning of fossil fuels since the Industrial Revolution.

Other Observed Trends

  • Rising sea levels: Global sea level has risen by about 20 cm since 1900, and the rate is accelerating.
  • Shrinking ice: Arctic sea ice is declining rapidly. Glaciers and ice sheets in Greenland and Antarctica are losing mass.
  • Changing rainfall patterns: Some areas are getting wetter, others drier. Extreme rainfall events are becoming more frequent.
  • More extreme weather: Heatwaves, droughts, floods, and tropical storms are increasing in frequency and intensity.
  • Ocean acidification: The oceans absorb about 25% of human-emitted $\text{CO}_2$, making the water more acidic and threatening marine life.
Exam Note: For exams, remember these key numbers: $1.1°C$ warming since pre-industrial era, $\text{CO}_2$ rose from 280 ppm to over 420 ppm (50% increase), sea level rose about 20 cm since 1900. These are the most frequently tested statistics.

Practice Questions — Trends

Q4. Calculate the percentage increase in atmospheric $\text{CO}_2$ concentration from pre-industrial levels (280 ppm) to the current level of approximately 420 ppm.

Answer:
Step 1: Identify the values.
Original (pre-industrial) = $280$ ppm
Current = $420$ ppm
Increase = $420 – 280 = 140$ ppm

Step 2: Calculate percentage increase.
$$\text{Percentage increase} = \frac{\text{Increase}}{\text{Original}} \times 100\%$$ $$= \frac{140}{280} \times 100\% = 0.5 \times 100\% = \mathbf{50\%}$$

Answer: The atmospheric $\text{CO}_2$ concentration has increased by approximately 50% since pre-industrial times.

Q5. List five observable trends that provide evidence of global climate change.

Answer:
1. Rising global average temperature — increased by about $1.1°C$ since pre-industrial era
2. Rising atmospheric $\text{CO}_2$ concentration — from 280 ppm to over 420 ppm
3. Rising sea levels — about 20 cm since 1900, with accelerating rate
4. Shrinking Arctic sea ice and glaciers — rapid decline in ice cover
5. Increased frequency and intensity of extreme weather events — heatwaves, droughts, floods, storms
(Other valid answers: changing rainfall patterns, ocean acidification, thawing permafrost)

2.3 Natural and Human Induced Climate Change

Not all climate change is caused by humans. The Earth’s climate has changed naturally throughout its history. But what is different now? Let us understand both types of causes.

Natural Causes of Climate Change

The Earth’s climate has changed many times in the past due to natural factors:

1. Volcanic Eruptions: Large volcanic eruptions release huge amounts of ash and sulfur dioxide ($\text{SO}_2$) into the atmosphere. These particles form an aerosol layer that reflects sunlight back into space, causing a temporary cooling effect. For example, the 1991 eruption of Mount Pinatubo caused global temperatures to drop by about $0.5°C$ for about two years.

2. Solar Variability: The amount of energy the Sun emits changes over time in cycles (approximately 11-year sunspot cycles). When the Sun is more active, slightly more energy reaches Earth, causing some warming. However, solar changes alone cannot explain the rapid warming observed since the mid-20th century.

3. Orbital Changes (Milankovitch Cycles): The Earth’s orbit around the Sun changes over tens of thousands of years in three ways: changes in eccentricity (shape of orbit), obliquity (tilt of Earth’s axis), and precession (wobble of the axis). These cycles are responsible for the coming and going of ice ages over geological time scales.

4. Natural Greenhouse Gas Variations: $\text{CO}_2$ levels have naturally varied between about 180 ppm (during ice ages) and 280 ppm (during warm periods) over the past 800,000 years. These changes were driven by natural processes, but they happened very slowly over thousands of years — NOT rapidly like today.

Human-Induced (Anthropogenic) Causes of Climate Change

The rapid climate change we are experiencing today is primarily driven by human activities. Let us study each cause carefully:

1. Burning of Fossil Fuels: This is the NUMBER ONE cause. When we burn coal, oil, and natural gas for energy (electricity, transport, industry), we release enormous amounts of $\text{CO}_2$ into the atmosphere. This has been the dominant source of the increased $\text{CO}_2$ since the Industrial Revolution.

2. Deforestation: Trees absorb $\text{CO}_2$ from the atmosphere through photosynthesis. When forests are cut down (for agriculture, logging, or urban expansion), this natural “carbon sink” is removed. Additionally, when trees are burned or decompose, the stored carbon is released back into the atmosphere.

3. Agriculture and Livestock: Rice paddies, cattle farming, and manure management produce significant amounts of methane ($\text{CH}_4$). Cows and sheep produce methane during digestion. The use of nitrogen-based fertilizers releases nitrous oxide ($\text{N}_2\text{O}$).

4. Industrial Processes: Manufacturing cement, chemicals, and metals releases $\text{CO}_2$ and other greenhouse gases. Industrial processes also produce CFCs and other synthetic greenhouse gases.

5. Urbanization: Cities produce the “urban heat island effect” — concrete and asphalt absorb heat, buildings block wind, and human activities (vehicles, air conditioning) generate additional heat. While this is more of a local effect, it contributes to the overall warming trend.

6. Waste Disposal: Landfills produce methane as organic waste decomposes without oxygen (anaerobic decomposition).

Key Point: While natural factors have caused climate changes in the past, they cannot explain the RAPID warming of the past 50–60 years. The scientific evidence shows that human activities — especially burning fossil fuels — are responsible for virtually ALL of the observed warming since the mid-20th century. Natural factors alone would have caused a slight cooling, not warming!
Exam Note: When asked to compare natural and human causes, remember: Natural causes operate over long time scales (thousands to millions of years) except for volcanic eruptions (which cause temporary cooling). Human causes operate over short time scales (decades) and cause sustained warming. The KEY distinction is the SPEED and DIRECTION of change.

Practice Questions — Causes

Q6. Explain how burning fossil fuels contributes to the enhanced greenhouse effect.

Answer: Fossil fuels (coal, oil, natural gas) are formed from the remains of ancient plants and animals that stored carbon underground over millions of years. When we burn these fuels, the chemical reaction releases carbon dioxide ($\text{CO}_2$) into the atmosphere. For example:
$$\text{C} + \text{O}_2 \rightarrow \text{CO}_2 + \text{energy}$$ This additional $\text{CO}_2$ accumulates in the atmosphere and enhances the greenhouse effect by absorbing more infrared radiation that would otherwise escape to space. Since the Industrial Revolution, burning fossil fuels has added over 1,500 billion tonnes of $\text{CO}_2$ to the atmosphere, making it the single largest contributor to the enhanced greenhouse effect.
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Q7. Why do volcanic eruptions typically cause short-term COOLING rather than warming?

Answer: Although volcanic eruptions release $\text{CO}_2$ (a greenhouse gas), they also release enormous amounts of ash and sulfur dioxide ($\text{SO}_2$). These particles form an aerosol layer in the stratosphere that acts like a shield, reflecting incoming solar radiation back into space before it reaches the Earth’s surface. This reflection effect (increased albedo) is stronger than the warming from the small amount of $\text{CO}_2$ released. The result is a net cooling effect that typically lasts 1–3 years. For example, the 1991 Mount Pinatubo eruption lowered global temperatures by about $0.5°C$ for approximately two years.

Q8. “Deforestation is a double problem for climate change.” Explain this statement.

Answer: Deforestation is a “double problem” because it affects climate change in TWO negative ways:

First (removing a carbon sink): Trees absorb $\text{CO}_2$ from the atmosphere through photosynthesis. When forests are cut down, this natural mechanism for removing $\text{CO}_2$ is lost, meaning more $\text{CO}_2$ stays in the atmosphere.

Second (releasing stored carbon): When trees are cut and either burned or left to decompose, the carbon that was stored in their biomass (trunks, branches, leaves, roots) is released back into the atmosphere as $\text{CO}_2$ or methane. This ADDS to the greenhouse gases in the atmosphere.

So deforestation both reduces the Earth’s ability to remove $\text{CO}_2$ AND releases additional $\text{CO}_2$ — a double negative effect.

2.4 Consequences of Climate Change

Climate change affects almost every aspect of our lives and the natural environment. Let us look at the major consequences one by one. As you read, think about which of these consequences are most relevant to Ethiopia.

1. Rising Temperatures and Heatwaves

As global temperatures rise, heatwaves become more frequent, more intense, and last longer. This can cause heat-related illnesses and deaths, reduce agricultural productivity, increase water demand, and strain energy supplies (more air conditioning needed).

2. Changing Rainfall Patterns

Climate change alters the water cycle, leading to changes in when, where, and how much rain falls. Some regions experience more intense rainfall and flooding, while others experience prolonged droughts. For Ethiopia, this is particularly concerning because agriculture is heavily dependent on rainfall.

3. Rising Sea Levels

Sea levels rise due to two main factors:

  • Thermal expansion: As ocean water warms, it expands (takes up more volume).
  • Melting ice: Melting glaciers and ice sheets (especially Greenland and Antarctica) add more water to the oceans.

Rising sea levels threaten coastal communities, infrastructure, and ecosystems through flooding, erosion, and saltwater intrusion into freshwater supplies.

4. Melting Ice and Glaciers

Arctic sea ice, mountain glaciers, and the ice sheets of Greenland and Antarctica are all melting at accelerating rates. This not only contributes to sea level rise but also disrupts ecosystems and the livelihoods of people who depend on glacial meltwater for freshwater.

5. More Extreme Weather Events

Climate change increases the frequency and intensity of extreme weather events including:

  • Tropical cyclones and hurricanes (warmer oceans provide more energy)
  • Heavy rainfall and flooding (warmer air holds more moisture)
  • Droughts (changing rainfall patterns and increased evaporation)
  • Wildfires (hotter, drier conditions)

6. Impact on Agriculture and Food Security

Climate change threatens food security by:

  • Reducing crop yields due to heat stress and water scarcity
  • Shifting growing seasons and suitable areas for different crops
  • Increasing pest and disease outbreaks
  • Reducing livestock productivity due to heat stress

For Ethiopia, where over 80% of the population depends on rain-fed agriculture, this is a critical concern.

7. Impact on Water Resources

Changes in rainfall patterns, accelerated glacier melt, and increased evaporation affect freshwater availability. Many regions, including parts of Ethiopia, may face increased water scarcity.

8. Impact on Human Health

  • Heat-related illnesses and deaths
  • Spread of vector-borne diseases (malaria, dengue) to new areas as temperatures warm
  • Respiratory problems from increased air pollution and wildfires
  • Malnutrition from reduced food production
  • Mental health impacts from displacement and disaster trauma

9. Impact on Biodiversity and Ecosystems

Many species cannot adapt quickly enough to changing conditions. Climate change causes habitat loss, shifts in species distribution, altered migration patterns, and increased extinction risk. Coral reefs are particularly vulnerable — warming oceans cause coral bleaching and death.

10. Socioeconomic Consequences

  • Climate refugees and migration (people displaced by sea level rise, drought, or extreme events)
  • Economic losses from damage to infrastructure and reduced agricultural output
  • Increased poverty and inequality (poor communities are most vulnerable)
  • Potential for conflicts over diminishing resources (water, arable land)
Key Point for Ethiopian Students: Ethiopia is highly vulnerable to climate change because: (1) most agriculture is rain-fed, (2) many people live in poverty with limited capacity to adapt, (3) the country already experiences frequent droughts and floods, and (4) ecosystems like the Ethiopian Highlands are sensitive to temperature changes. Understanding these consequences is essential for your exam!
Exam Note: When listing consequences, always try to give SPECIFIC examples relevant to Ethiopia. For example, instead of just saying “reduced agriculture,” say “reduced cereal crop yields (teff, maize, wheat) due to erratic rainfall in the Ethiopian Highlands.” This shows deeper understanding.

Practice Questions — Consequences

Q9. Explain the two main reasons why sea levels are rising due to climate change.

Answer:
1. Thermal expansion of ocean water: As the oceans absorb heat from global warming, the water molecules gain kinetic energy and move further apart. This causes the water to expand in volume (take up more space), leading to higher sea levels even without any additional water being added.

2. Melting of land-based ice: Glaciers, ice caps, and the ice sheets of Greenland and Antarctica are melting at accelerating rates due to rising temperatures. This meltwater flows into the oceans, adding to the total volume of water and raising sea levels. (Note: melting of sea ice does NOT directly raise sea levels because it is already floating in the ocean.)

Both factors are happening simultaneously, and both are accelerating as temperatures continue to rise.

Q10. Why is Ethiopia particularly vulnerable to the impacts of climate change? Give three reasons.

Answer:
1. Dependence on rain-fed agriculture: Over 80% of Ethiopia’s population depends on agriculture, and most of this agriculture relies on seasonal rainfall rather than irrigation. Changes in rainfall patterns directly threaten food production and livelihoods.

2. High poverty levels: Limited financial resources mean that communities and the government have less capacity to invest in adaptation measures such as irrigation infrastructure, drought-resistant crops, and early warning systems.

3. Existing climate variability: Ethiopia already experiences frequent droughts and floods. Climate change is expected to make these events more frequent and severe, pushing an already vulnerable system beyond its coping capacity.

(Other valid reasons: sensitive highland ecosystems, limited access to technology and information, high population growth increasing pressure on resources.)

Q11. How does climate change affect the spread of diseases like malaria? Explain the mechanism.

Answer: Climate change affects the spread of malaria by changing the conditions that mosquitoes (the vector) need to survive and reproduce:

1. Warmer temperatures: Mosquitoes thrive in warm conditions. As temperatures rise, areas that were previously too cold for mosquitoes become suitable for their survival. This expands the geographic range where malaria can be transmitted. Warmer temperatures also speed up the mosquito life cycle, allowing more generations per year.

2. Changed rainfall patterns: Mosquitoes breed in standing water. Increased rainfall in some areas creates more breeding sites, while droughts can also create stagnant water pools. Both scenarios can increase mosquito populations.

3. Shorter development time of the parasite: The malaria parasite develops faster inside the mosquito at warmer temperatures, making mosquitoes infectious more quickly.

Result: Malaria may spread to highland areas of Ethiopia (such as parts of Amhara and Oromia) that were previously malaria-free.

2.5 Adaptation and Mitigation Strategies to Climate Change

Now that we understand the problem, what can we do about it? There are two main approaches: adaptation and mitigation. Do you know the difference? Let us learn!

Adaptation

Adaptation means adjusting to the actual or expected effects of climate change. It is about learning to LIVE with the changes that are already happening or that we cannot avoid. Adaptation reduces vulnerability and builds resilience.

Examples of adaptation strategies:

  • Agricultural adaptation: Planting drought-resistant crop varieties, changing planting dates, practicing crop diversification, using irrigation systems instead of relying only on rain
  • Water management: Building water harvesting structures (ponds, dams), improving water use efficiency, rainwater harvesting
  • Infrastructure: Building flood defenses, strengthening buildings against extreme weather, elevating roads in flood-prone areas
  • Health systems: Strengthening disease surveillance, establishing early warning systems for heatwaves and disease outbreaks
  • Ecosystem-based adaptation: Restoring mangroves to protect coastlines, reforestation to prevent soil erosion and regulate water flow
  • Community-level adaptation: Diversifying livelihoods, community-based disaster risk reduction, traditional knowledge practices

Mitigation

Mitigation means reducing the emission of greenhouse gases or increasing carbon sinks to reduce the magnitude of climate change. It is about addressing the ROOT CAUSE — stopping the problem from getting worse.

Examples of mitigation strategies:

  • Energy: Shifting from fossil fuels to renewable energy sources (solar, wind, hydro, geothermal), improving energy efficiency
  • Transportation: Promoting public transport, electric vehicles, cycling, and walking instead of private car use
  • Forestry: Reducing deforestation, afforestation (planting new forests), reforestation (replanting degraded forests)
  • Agriculture: Improved livestock management to reduce methane emissions, better fertilizer management to reduce $\text{N}_2\text{O}$, practices that increase soil carbon storage
  • Industry: Using cleaner production technologies, carbon capture and storage (CCS)
  • Waste management: Capturing methane from landfills, recycling, composting organic waste
Key Point: Adaptation = dealing with the EFFECTS (living with it). Mitigation = dealing with the CAUSES (stopping it from getting worse). BOTH are needed! We must mitigate to prevent the worst scenarios, AND adapt to the changes that are already unavoidable. Think of it this way: mitigation reduces the flood, adaptation builds a boat.
Exam Note: When asked about Ethiopia’s strategies, remember Ethiopia has a strong policy framework — the Climate Resilient Green Economy (CRGE) strategy (discussed in Section 2.7). For adaptation, focus on agriculture (drought-resistant crops, irrigation), water harvesting, and early warning systems. For mitigation, focus on renewable energy (hydro, geothermal, solar), reforestation (Green Legacy Initiative), and reducing deforestation.

Practice Questions — Adaptation and Mitigation

Q12. Differentiate between climate change adaptation and mitigation. Give one example of each that is relevant to Ethiopia.

Answer:
Adaptation = Adjusting to the effects of climate change to reduce vulnerability. It does not reduce greenhouse gas emissions but helps communities cope with changes.
Ethiopian example: Planting drought-resistant crop varieties (e.g., improved sorghum and teff varieties) to cope with increasing drought frequency.

Mitigation = Reducing greenhouse gas emissions or increasing carbon sinks to address the root cause of climate change.
Ethiopian example: Expanding renewable energy generation (such as the Grand Ethiopian Renaissance Dam for hydropower, or geothermal energy development in the Rift Valley) to reduce dependence on fossil fuels and reduce $\text{CO}_2$ emissions.

Key distinction: Adaptation manages the impacts; mitigation reduces the causes. Both are necessary.

Q13. Explain why afforestation is considered both an adaptation and a mitigation strategy.

Answer:
As a mitigation strategy: Trees absorb $\text{CO}_2$ from the atmosphere through photosynthesis, storing carbon in their biomass (trunks, branches, roots) and in the soil. This directly reduces the concentration of greenhouse gases in the atmosphere, addressing the root cause of climate change.

As an adaptation strategy: Forests provide ecosystem services that help communities adapt to climate change impacts. These include: regulating local water cycles (reducing flood risk and improving water availability), preventing soil erosion, providing shade that reduces local temperatures, protecting biodiversity, and supplying alternative livelihoods (fruits, nuts, medicine, timber) that diversify income sources when crops fail due to drought.

This “double benefit” makes afforestation one of the most cost-effective climate strategies.

2.6 International Conventions and Agreements on Climate

Climate change is a global problem that no single country can solve alone. That is why countries around the world have come together to create international agreements. Let us learn about the most important ones!

1. The United Nations Framework Convention on Climate Change (UNFCCC)

Established in 1992 at the Earth Summit in Rio de Janeiro, Brazil. It is the foundational international treaty on climate change. Key features:

  • Recognized that climate change is a serious global problem
  • Established the principle of “common but differentiated responsibilities” — all countries have a shared responsibility, but developed countries (which historically emitted the most GHGs) should take the lead
  • Set the ultimate objective of stabilizing greenhouse gas concentrations at a level that would prevent dangerous human interference with the climate system
  • Has been ratified by virtually every country in the world (nearly 200 parties)

2. The Kyoto Protocol (1997)

Adopted in 1997 in Kyoto, Japan. It was the first legally binding international agreement to reduce greenhouse gas emissions. Key features:

  • Set specific emission reduction targets for developed (Annex I) countries only
  • Developing countries (including Ethiopia) were NOT required to reduce emissions
  • Compliance mechanisms were established
  • The first commitment period was 2008–2012
  • The United States never ratified it, and Canada withdrew
  • Had limited effectiveness due to these issues

3. The Paris Agreement (2015)

Adopted in 2015 at the COP21 conference in Paris, France. This is currently the most important global climate agreement. Key features:

  • Universal participation: Unlike Kyoto, ALL countries (developed AND developing) make commitments to reduce emissions
  • Temperature targets: The central aim is to keep global temperature rise this century well below $2°C$ above pre-industrial levels, and to pursue efforts to limit it to $1.5°C$
  • Nationally Determined Contributions (NDCs): Each country sets its own climate action plan (NDC) specifying how it will reduce emissions and adapt to climate change
  • 5-year cycle: Countries update and strengthen their NDCs every 5 years
  • Climate finance: Developed countries committed to providing $100 billion per year to help developing countries with mitigation and adaptation
  • Entered into force in 2016 — remarkably fast for an international treaty
$$\text{Paris Agreement Temperature Targets:}$$ $$\text{Goal 1: } \Delta T < 2°C \text{ above pre-industrial levels}$$ $$\text{Goal 2: Pursue } \Delta T \leq 1.5°C \text{ above pre-industrial levels}$$
Exam Note: Know the year, location, and key feature of each agreement:
UNFCCC (1992, Rio) — framework treaty, “common but differentiated responsibilities”
Kyoto Protocol (1997, Kyoto) — legally binding targets for developed countries only
Paris Agreement (2015, Paris) — universal participation, NDCs, well below $2°C$ / pursue $1.5°C$, $100 billion/year climate finance

Practice Questions — International Agreements

Q14. What is the principle of “common but differentiated responsibilities” and why is it important in international climate agreements?

Answer: The principle of “common but differentiated responsibilities” (CBDR) means that ALL countries share a common responsibility to address climate change (because it is a global problem), BUT the responsibility is differentiated (different) based on each country’s historical contribution to the problem and its capacity to respond.

Why it is important:
• Developed countries (like the USA, UK, Germany) have been burning fossil fuels since the Industrial Revolution and are responsible for the MAJORITY of cumulative GHG emissions in the atmosphere. They also have greater financial and technological capacity to address the problem.
• Developing countries (like Ethiopia) have contributed very little to historical emissions but are often the most vulnerable to climate change impacts and have fewer resources to adapt.
• Without this principle, developing countries would be unfairly burdened with obligations they cannot afford, while the countries most responsible would escape their fair share of the effort. This principle ensures fairness in global climate action.

Q15. Compare the Kyoto Protocol and the Paris Agreement in terms of country participation and approach to emission reductions.

Answer:
Kyoto Protocol (1997):
• Only developed (Annex I) countries were required to reduce emissions
• Developing countries had no binding emission reduction obligations
• Used a “top-down” approach — targets were set internationally and imposed on countries
• Limited effectiveness — the US never ratified, Canada withdrew

Paris Agreement (2015):
• ALL countries (developed and developing) make commitments
• Each country determines its own targets through Nationally Determined Contributions (NDCs)
• Uses a “bottom-up” approach — countries set their own goals based on their circumstances
• Much broader participation — nearly universal

Key difference: Kyoto was top-down with targets only for rich countries; Paris is bottom-up with self-determined targets for ALL countries. This is why Paris achieved much wider participation.

2.7 Pillars of Climate Resilient Green Economy (CRGE) of Ethiopia

Now let us look at what Ethiopia is specifically doing about climate change. This is very important for your exam because questions about Ethiopia’s climate policy come up frequently!

Ethiopia launched its Climate Resilient Green Economy (CRGE) strategy in 2011. The CRGE has two main goals:

  1. Mitigation: Achieve middle-income status through green growth (reducing GHG emissions while growing the economy)
  2. Adaptation: Build resilience to the impacts of climate change

The CRGE strategy is built on four pillars:

Pillar 1: Improving Crop and Livestock Production Practices

This focuses on agricultural adaptation and mitigation:

  • Promoting drought-resistant and high-yielding crop varieties
  • Improving soil fertility and water management
  • Reducing emissions from livestock (better feed, manure management)
  • Expanding small-scale irrigation
  • Shifting from traditional to modern agricultural practices

Pillar 2: Protecting and Restoring Forests

This focuses on the forestry sector as a carbon sink:

  • Reducing deforestation (the main source of Ethiopia’s $\text{CO}_2$ emissions)
  • Reforestation and afforestation programs
  • Sustainable forest management
  • The Green Legacy Initiative (planting billions of seedlings) is a recent example

Pillar 3: Scaling Up Renewable Energy

This focuses on clean energy development:

  • Expanding hydropower (e.g., Grand Ethiopian Renaissance Dam — GERD)
  • Developing geothermal energy (especially in the Rift Valley)
  • Promoting solar and wind energy
  • Improving energy efficiency
  • Expanding electricity access to rural areas

Pillar 4: Using Energy-Efficient Technologies in Transport, Industry, and Buildings

This focuses on reducing energy demand and emissions from non-agricultural sectors:

  • Promoting fuel-efficient vehicles and public transport
  • Using energy-efficient industrial processes
  • Building energy-efficient homes and buildings
  • Reducing reliance on biomass (wood, charcoal) for cooking and heating
  • Promoting clean cooking technologies (e.g., biogas, electric stoves)
Key Point: Ethiopia’s CRGE strategy is unique because it treats climate change as an OPPORTUNITY rather than just a problem. Instead of choosing between economic growth and environmental protection, the CRGE aims to achieve BOTH — growing the economy while reducing emissions and building resilience. The four pillars (agriculture, forestry, renewable energy, energy efficiency) cover the main sectors of Ethiopia’s economy.
Exam Note: Memorize the four CRGE pillars:
1. Improving crop and livestock production practices
2. Protecting and restoring forests
3. Scaling up renewable energy
4. Using energy-efficient technologies in transport, industry, and buildings

Also remember: CRGE was launched in 2011, has TWO goals (green growth + resilience), and Ethiopia aims to achieve middle-income status through this strategy.

Practice Questions — CRGE

Q16. State the four pillars of Ethiopia’s Climate Resilient Green Economy (CRGE) strategy and give one specific action under each pillar.

Answer:
Pillar 1 — Improving crop and livestock production practices: Example: Expanding small-scale irrigation to reduce dependence on rain-fed agriculture.

Pillar 2 — Protecting and restoring forests: Example: The Green Legacy Initiative, which involves planting billions of tree seedlings across the country to restore degraded lands and increase carbon sequestration.

Pillar 3 — Scaling up renewable energy: Example: Developing the Grand Ethiopian Renaissance Dam (GERD) for hydropower generation, or exploiting geothermal energy resources in the Ethiopian Rift Valley.

Pillar 4 — Using energy-efficient technologies in transport, industry, and buildings: Example: Promoting clean cooking technologies (such as biogas or electric stoves) to reduce reliance on biomass fuels (wood and charcoal) that cause deforestation and indoor air pollution.

Q17. Why is Ethiopia’s CRGE strategy described as treating climate change as an “opportunity” rather than just a “problem”?

Answer: The CRGE strategy treats climate change as an opportunity because it recognizes that Ethiopia can achieve ECONOMIC GROWTH while simultaneously addressing climate change. Specifically:

1. Ethiopia has enormous untapped renewable energy potential (hydropower, geothermal, solar, wind) that can power industrialization without increasing emissions — this is a competitive advantage.
2. Improving agricultural practices can increase food production AND build resilience to drought — solving two problems at once.
3. Reforestation can provide timber, non-timber forest products, and ecosystem services while sequestering carbon.
4. Energy-efficient technologies can reduce costs for businesses and households while reducing emissions.

Instead of seeing climate action as a cost that slows development, the CRGE sees it as a PATHWAY to sustainable development — hence it is an “opportunity” for Ethiopia to leapfrog to a green economy.

Unit Summary Review

Q18. Briefly describe the complete chain from human activities to climate change consequences, using the following terms: fossil fuels, greenhouse effect, $\text{CO}_2$, global warming, climate change, consequences.

Answer:
Step 1: Human activities (especially burning fossil fuels like coal, oil, and natural gas) release large amounts of $\text{CO}_2$ and other greenhouse gases into the atmosphere.
Step 2: These additional gases enhance the natural greenhouse effect — more infrared radiation is trapped in the atmosphere.
Step 3: The enhanced greenhouse effect causes the Earth’s average surface temperature to rise — this is global warming.
Step 4: Global warming leads to broader changes in the Earth’s climate system — changes in rainfall, sea level, extreme events, etc. — this is climate change.
Step 5: Climate change produces various consequences: rising temperatures, changing rainfall patterns, rising sea levels, melting ice, more extreme weather, reduced agriculture, health impacts, biodiversity loss, and socioeconomic problems.

This chain shows how human actions at the source ultimately affect every aspect of life on Earth.

Revision Notes — Exam Focus

Important Definitions

TermDefinition
WeatherShort-term atmospheric conditions at a specific place and time (hours to weeks).
ClimateLong-term average of weather conditions over 30 or more years.
Climate ChangeSignificant and lasting changes in weather patterns over decades to millions of years; in modern context, largely attributed to human activities.
Global WarmingThe increase in Earth’s average surface temperature; one aspect of climate change.
Greenhouse EffectNatural process where GHGs trap heat in the atmosphere, keeping Earth warm enough for life.
Enhanced Greenhouse EffectThe intensified greenhouse effect caused by human-increased GHG concentrations.
Greenhouse Gases (GHGs)Gases that absorb and re-emit infrared radiation: $\text{CO}_2$, $\text{CH}_4$, $\text{N}_2\text{O}$, CFCs, water vapor.
AdaptationAdjusting to actual or expected climate change effects to reduce vulnerability.
MitigationReducing GHG emissions or increasing carbon sinks to reduce the magnitude of climate change.
NDCsNationally Determined Contributions — each country’s self-set climate action plan under the Paris Agreement.
CRGEClimate Resilient Green Economy — Ethiopia’s national strategy for green growth and climate resilience (launched 2011).
CBDRCommon But Differentiated Responsibilities — principle that all countries share responsibility but developed countries take the lead.
Thermal ExpansionThe increase in volume of ocean water as it warms, contributing to sea level rise.
Carbon SinkA natural system (forest, ocean) that absorbs more carbon than it releases.
AfforestationPlanting trees on land that was not previously forested.
ReforestationReplanting trees on land that was previously forested but has been cleared.

Key Formulas and Calculations

1. Percentage Increase Calculation:
$$\text{Percentage increase} = \frac{\text{New value} – \text{Original value}}{\text{Original value}} \times 100\%$$
Example: $\text{CO}_2$ increased from 280 ppm to 420 ppm:
$$\frac{420 – 280}{280} \times 100\% = \frac{140}{280} \times 100\% = 50\%$$
2. GHG Potency Comparison:
$$\text{Methane is about } 25\times \text{ more potent than } \text{CO}_2 \text{ (over 100 years)}$$ $$\text{Nitrous oxide is about } 300\times \text{ more potent than } \text{CO}_2 \text{ (over 100 years)}$$
Example: If 1 tonne of $\text{CO}_2$ causes 1 unit of warming, then 1 tonne of $\text{CH}_4$ causes 25 units, and 1 tonne of $\text{N}_2\text{O}$ causes 300 units.
3. Paris Agreement Temperature Targets:
$$\text{Target 1: } \Delta T < 2°C \text{ above pre-industrial levels}$$ $$\text{Target 2: Pursue } \Delta T \leq 1.5°C \text{ above pre-industrial levels}$$

Key Statistics to Memorize

  • Global warming since pre-industrial era: ~$1.1°C$
  • Pre-industrial $\text{CO}_2$: 280 ppm → Current: over 420 ppm (50% increase)
  • Sea level rise since 1900: ~20 cm
  • $\text{CO}_2$ contribution to anthropogenic warming: ~76%
  • Methane contribution: ~16%
  • Nitrous oxide contribution: ~6%
  • Paris Agreement year: 2015
  • UNFCCC year: 1992
  • Kyoto Protocol year: 1997
  • CRGE launched: 2011
  • Climate finance commitment: $100 billion/year from developed countries
  • NDC update cycle: every 5 years

International Agreements — Quick Comparison

FeatureUNFCCC (1992)Kyoto Protocol (1997)Paris Agreement (2015)
LocationRio de JaneiroKyoto, JapanParis, France
NatureFramework treatyLegally binding targetsLegally binding process (not targets)
Who reduces?Developed leadDeveloped only (Annex I)ALL countries
ApproachPrinciples & frameworkTop-down targetsBottom-up (NDCs)
Key PrincipleCBDRBinding targets for richUniversal NDCs, $<2°C$ / $1.5°C$

CRGE Four Pillars — Quick List

1. Improving crop and livestock production practices (agriculture)
2. Protecting and restoring forests (forestry)
3. Scaling up renewable energy (energy)
4. Using energy-efficient technologies in transport, industry, and buildings (efficiency)

Natural vs. Human Causes — Quick Comparison

FeatureNatural CausesHuman (Anthropogenic) Causes
Time scaleThousands to millions of years (except volcanoes)Decades (rapid)
DirectionCan cause warming OR coolingCauses sustained warming
Current roleCannot explain recent rapid warmingResponsible for virtually ALL recent warming
ExamplesVolcanic eruptions, solar variability, Milankovitch cyclesFossil fuel burning, deforestation, agriculture, industry

Common Mistakes to Avoid

  1. Confusing weather and climate: Weather = short-term; Climate = long-term average (30+ years)
  2. Saying global warming and climate change are the same: Global warming is about temperature only; climate change includes all effects (rainfall, sea level, extremes, etc.)
  3. Saying the greenhouse effect is entirely bad: The NATURAL greenhouse effect is essential for life. It is the ENHANCED greenhouse effect that is the problem
  4. Forgetting water vapor is a GHG: Water vapor IS the most abundant GHG, but human activities do not directly control it
  5. Saying volcanic eruptions cause global warming: They cause SHORT-TERM COOLING (aerosol effect), not warming
  6. Confusing adaptation and mitigation: Adaptation = coping with effects; Mitigation = reducing causes
  7. Saying the Kyoto Protocol included all countries: It only required emission reductions from developed (Annex I) countries
  8. Confusing the Paris Agreement temperature targets: Well below $2°C$ AND pursue $1.5°C$ — both targets exist
  9. Saying melting sea ice raises sea levels: Sea ice is already floating; melting LAND ice (glaciers, ice sheets) raises sea levels
  10. Forgetting CRGE has TWO goals: Both green growth (mitigation) AND resilience (adaptation)
  11. Saying Ethiopia has no role in mitigation: Under the Paris Agreement, ALL countries (including Ethiopia) have NDCs

Adaptation vs. Mitigation Examples — Quick Reference

Adaptation (Cope with effects)Mitigation (Reduce causes)
Drought-resistant cropsSolar power plants
Irrigation systemsAfforestation/reforestation
Flood defenses / leveesPublic transport systems
Early warning systemsGeothermal energy development
Heat action plansReducing deforestation
Climate-resilient infrastructureImproved cookstoves (reduce biomass use)
Disease surveillance systemsCarbon capture and storage
Water harvesting structuresIndustrial efficiency improvements

Challenge Exam Questions

These questions are designed to test your deep understanding. Try each one before looking at the answer. Good luck!

Multiple Choice Questions

Q1. Which of the following is the MOST significant contributor to the enhanced greenhouse effect?

A) Water vapor
B) Methane from agriculture
C) Carbon dioxide from burning fossil fuels
D) Nitrous oxide from fertilizers

Answer: C
Carbon dioxide from burning fossil fuels is the single largest contributor to the enhanced greenhouse effect, accounting for approximately 76% of anthropogenic greenhouse gas emissions. While water vapor is the most abundant GHG overall, its concentration is primarily controlled by natural processes (temperature), not directly by human activities. Methane (16%) and nitrous oxide (6%) are significant but secondary.

Q2. The principle of “common but differentiated responsibilities” was first established in which international agreement?

A) Kyoto Protocol, 1997
B) Paris Agreement, 2015
C) UNFCCC, 1992
D) Montreal Protocol, 1987

Answer: C
The principle of “common but differentiated responsibilities” (CBDR) was first established in the United Nations Framework Convention on Climate Change (UNFCCC) in 1992 at the Earth Summit in Rio de Janeiro. This foundational principle was then carried forward into subsequent agreements like the Kyoto Protocol and the Paris Agreement. The Montreal Protocol (1987) dealt with ozone-depleting substances, not climate change.

Q3. If the concentration of $\text{CO}_2$ in the atmosphere increased from 300 ppm to 450 ppm, what is the percentage increase?

A) 30%
B) 50%
C) 150%
D) 33%

Answer: B
$$\text{Percentage increase} = \frac{450 – 300}{300} \times 100\% = \frac{150}{300} \times 100\% = 0.5 \times 100\% = 50\%$$
The $\text{CO}_2$ concentration increased by 50%. Note that this is the same percentage increase as the actual pre-industrial to current change (280 to 420 ppm) because the ratio of increase to original is the same ($150/300 = 140/280 = 0.5$).

Q4. Which of the following is an example of BOTH adaptation and mitigation?

A) Building a flood wall
B) Installing solar panels
C) Planting trees
D) Using drought-resistant seeds

Answer: C
Planting trees (afforestation/reforestation) serves as BOTH adaptation and mitigation:
Mitigation: Trees absorb $\text{CO}_2$, reducing GHG concentrations (addressing the cause)
Adaptation: Trees regulate water cycles, prevent erosion, provide shade, and support biodiversity (helping cope with effects)

Options A and D are adaptation only. Option B is mitigation only.

Q5. Under the Paris Agreement, how often are countries required to update their Nationally Determined Contributions (NDCs)?

A) Every year
B) Every 3 years
C) Every 5 years
D) Every 10 years

Answer: C
Under the Paris Agreement, countries are required to update and strengthen their NDCs every 5 years. This ratchet mechanism is designed to ensure that global climate action becomes more ambitious over time, as the initial NDCs were not sufficient to meet the $2°C$ or $1.5°C$ targets.

Fill in the Blank

Q6. The difference between weather and climate is that weather refers to __________ conditions, while climate refers to __________ conditions averaged over __________ years or more.

Answer: short-term; long-term; 30

Weather describes atmospheric conditions over hours to weeks. Climate is the statistical average of weather over a period of at least 30 years, as defined by the World Meteorological Organization (WMO).

Q7. Without the natural greenhouse effect, Earth’s average surface temperature would be approximately __________°C instead of the current average of about __________°C.

Answer: -18; +15

The natural greenhouse effect keeps Earth about $33°C$ warmer than it would otherwise be ($15 – (-18) = 33°C$). This natural warming is essential for life. The problem is the ENHANCED greenhouse effect caused by human activities.

Q8. Methane ($\text{CH}_4$) is approximately __________ times more potent than $\text{CO}_2$ at trapping heat over a 100-year period.

Answer: 25

Methane has a Global Warming Potential (GWP) of about 25 over a 100-year period, meaning one tonne of methane traps about 25 times more heat than one tonne of $\text{CO}_2$ over that period. Over a 20-year period, it is even more potent (about 84 times).

Q9. The two main physical processes causing sea level rise are __________ expansion of ocean water and __________ of land-based ice.

Answer: thermal; melting

Thermal expansion occurs because water expands as it warms. Melting of glaciers, ice caps, and the Greenland and Antarctic ice sheets adds water volume to the oceans. Note: melting of floating sea ice does NOT directly raise sea levels.

Q10. Ethiopia’s Climate Resilient Green Economy (CRGE) strategy was launched in the year __________ and is built on __________ pillars.

Answer: 2011; four

The CRGE strategy was launched in 2011 and is structured around four pillars: (1) improving crop and livestock production, (2) protecting and restoring forests, (3) scaling up renewable energy, and (4) using energy-efficient technologies in transport, industry, and buildings.

Short Answer Questions

Q11. Explain why the enhanced greenhouse effect is primarily attributed to human activities rather than natural processes.

Answer: The enhanced greenhouse effect is attributed to human activities because:

1. The speed of change: Natural factors (Milankovitch cycles, solar variability) change $\text{CO}_2$ levels very slowly over thousands of years. The current 50% increase in $\text{CO}_2$ has occurred in just ~150 years — far too fast for natural processes.

2. The direction contradicts natural trends: Based on natural orbital cycles, the Earth should actually be cooling slightly right now, not warming rapidly.

3. The source is identifiable: The type of carbon in the atmosphere shows a “fingerprint” of fossil fuels (it contains less Carbon-14, which decays over millions of years while fossil fuels are underground).

4. Quantitative analysis: Scientific studies show that natural factors alone CANNOT explain the observed warming. Only when human GHG emissions are included do climate models match the observed temperature record.

5. Timing: The rapid warming began in the mid-20th century, exactly when fossil fuel use dramatically increased — not a coincidence.

Q12. Describe three specific ways in which climate change could affect agriculture in Ethiopia, and for each, suggest one adaptation strategy.

Answer:
Impact 1: Increased frequency of droughts reducing crop yields
Adaptation: Plant drought-resistant crop varieties (e.g., improved sorghum, millet) and expand small-scale irrigation to reduce dependence on rainfall.

Impact 2: Erratic rainfall patterns disrupting planting and harvesting schedules
Adaptation: Use early warning systems and seasonal climate forecasts to adjust planting dates, and practice crop diversification to spread risk across different crop types.

Impact 3: Increased pest and disease outbreaks due to warmer temperatures
Adaptation: Strengthen integrated pest management (IPM) programs, use resistant crop varieties, and improve disease surveillance and response systems.

(Other valid impacts: soil degradation from heavy rains, heat stress on livestock, reduced pasture availability)

Q13. Compare the effectiveness of the Kyoto Protocol and the Paris Agreement in addressing global climate change.

Answer:
Kyoto Protocol — limited effectiveness:
• Only required developed countries to reduce emissions — developing countries (including major emitters like China and India) had no obligations
• The US (then the largest emitter) never ratified it
• Canada withdrew in 2011
• Without the world’s biggest emitters participating, the overall impact on global emissions was minimal
• Used a top-down approach that was seen as inflexible

Paris Agreement — more effective (but still insufficient):
• Achieved universal participation — nearly every country in the world has submitted NDCs
• The bottom-up approach (countries set their own targets) made participation politically feasible
• Created a framework for increasing ambition over time (5-year ratchet mechanism)
• Included climate finance for developing countries ($100 billion/year commitment)
• However, current NDCs are still NOT sufficient to meet the $1.5°C$ target — more ambition is needed

Conclusion: The Paris Agreement is more effective than Kyoto in terms of participation and framework, but its actual effectiveness depends on whether countries strengthen their NDCs and implement them fully.

Q14. Explain the mechanism by which deforestation in the Ethiopian highlands could contribute to climate change AND worsen its local impacts.

Answer:
Contribution to climate change (global impact):
• Trees store carbon in their biomass. When forests are cleared, this stored carbon is released as $\text{CO}_2$ (if burned) or slowly through decomposition
• Ethiopia’s highlands have significant forest carbon stocks, and deforestation is a major source of Ethiopia’s GHG emissions
• Loss of forests removes a carbon sink, meaning less $\text{CO}_2$ is removed from the atmosphere in the future

Worsening local impacts:
• Without tree cover, rainfall runs off quickly instead of infiltrating the soil, leading to reduced groundwater recharge and more frequent water shortages (worsening drought impacts)
• Soil erosion increases without tree roots to hold soil, reducing soil fertility and agricultural productivity
• Loss of shade increases local temperatures, worsening heat stress on crops, livestock, and people
• Reduced biodiversity makes ecosystems less resilient to climate shocks
• Increased sedimentation in rivers and reservoirs reduces water storage capacity

This creates a vicious cycle: deforestation worsens climate change, and climate change makes the impacts of deforestation more severe.

Step-by-Step Calculation Questions

Q15. The atmospheric concentration of $\text{CO}_2$ was 315 ppm in 1960 and 420 ppm in 2023. Calculate the percentage increase and the average rate of increase per year.

Answer:
Part 1: Percentage increase
$$\text{Increase} = 420 – 315 = 105 \text{ ppm}$$ $$\text{Percentage increase} = \frac{105}{315} \times 100\% = \frac{1}{3} \times 100\% \approx \mathbf{33.3\%}$$

Part 2: Average rate of increase per year
$$\text{Number of years} = 2023 – 1960 = 63 \text{ years}$$ $$\text{Rate} = \frac{105 \text{ ppm}}{63 \text{ years}} \approx \mathbf{1.67 \text{ ppm per year}}$$

Interpretation: $\text{CO}_2$ increased by about 33.3% over 63 years, at an average rate of approximately 1.67 ppm per year. Note: the actual rate has been ACCELERATING — it is currently over 2.5 ppm/year, much faster than this historical average.

Q16. If methane is 25 times more potent than $\text{CO}_2$ over a 100-year period, how many tonnes of $\text{CO}_2$-equivalent would 4 tonnes of methane represent?

Answer:
Step 1: Identify the Global Warming Potential (GWP) of methane.
GWP of $\text{CH}_4$ = 25 (over 100 years)

Step 2: Multiply the mass of methane by its GWP.
$$\text{CO}_2\text{-equivalent} = \text{Mass of } \text{CH}_4 \times \text{GWP}$$ $$= 4 \text{ tonnes} \times 25 = \mathbf{100 \text{ tonnes of } \text{CO}_2\text{-equivalent}}$$

Interpretation: Releasing 4 tonnes of methane has the same warming effect as releasing 100 tonnes of $\text{CO}_2$ over a 100-year period. This shows why even small amounts of methane are very significant for climate change.

Q17. Country A emits 500 million tonnes of $\text{CO}_2$ per year and pledges to reduce this by 40% over 10 years. Country B emits 200 million tonnes of $\text{CO}_2$ per year and pledges to reduce this by 20% over 10 years. Which country reduces MORE $\text{CO}_2$ in absolute terms? Show your calculations.

Answer:
Country A:
Current emission = $500$ million tonnes
Reduction = $40\%$ of $500 = 0.40 \times 500 = \mathbf{200 \text{ million tonnes}}$
New emission = $500 – 200 = 300$ million tonnes

Country B:
Current emission = $200$ million tonnes
Reduction = $20\%$ of $200 = 0.20 \times 200 = \mathbf{40 \text{ million tonnes}}$
New emission = $200 – 40 = 160$ million tonnes

Comparison:
Country A reduces 200 million tonnes.
Country B reduces 40 million tonnes.
Country A reduces MORE in absolute terms (200 vs 40 million tonnes), even though Country B has a higher percentage reduction relative to its emissions.

Lesson: When comparing climate commitments, always look at both percentage AND absolute reductions. A large emitter making a modest percentage reduction may still cut more than a small emitter making a large percentage reduction.

Q18. If global temperature has already risen by $1.1°C$ and the Paris Agreement aims to keep it well below $2°C$, what is the maximum additional warming allowed? Express your answer as a temperature increase and as a percentage of the warming already experienced.

Answer:
Part 1: Maximum additional warming
$$\text{Maximum additional warming} = 2°C – 1.1°C = \mathbf{0.9°C}$$
(Using the “well below $2°C$” target as the upper bound)

Part 2: As a percentage of warming already experienced
$$\text{Percentage} = \frac{0.9}{1.1} \times 100\% \approx \mathbf{81.8\%}$$

Interpretation: We can only afford an additional $0.9°C$ of warming to stay within the Paris Agreement’s upper limit. This is about 82% of the warming that has already occurred — meaning we are very close to the limit. If we aim for the more ambitious $1.5°C$ target, the remaining “budget” is only $0.4°C$, which is just 36% of the warming already experienced!

More Difficult Questions

Q19. “Ethiopia’s contribution to global greenhouse gas emissions is very small, yet the country is among the most vulnerable to climate change impacts.” Discuss this statement, explaining why this situation is unfair and what international mechanisms exist to address it.

Answer:
Why Ethiopia’s emissions are small: Ethiopia is a developing country with low industrialization. Its per capita $\text{CO}_2$ emissions are among the lowest in the world (less than 0.1 tonnes per person per year, compared to over 15 tonnes for the US). Ethiopia’s total GHG emissions are a tiny fraction of global emissions.

Why Ethiopia is highly vulnerable:
• Over 80% of the population depends on rain-fed agriculture, which is highly sensitive to climate variability
• Frequent droughts and floods already cause significant damage
• Limited financial resources for adaptation
• High poverty levels reduce coping capacity
• Sensitive ecosystems (highlands, Rift Valley)

Why this is unfair: The countries that contributed the MOST to the problem (developed nations through 150+ years of fossil fuel use) are often the LEAST affected, while countries that contributed the LEAST (like Ethiopia) suffer the MOST. This is a fundamental injustice of climate change.

International mechanisms to address this:
1. Principle of CBDR in the UNFCCC — recognizes differentiated responsibility
2. Climate finance — developed countries committed $100 billion/year to help developing countries
3. Paris Agreement’s NDC system — allows different levels of ambition based on national circumstances
4. Green Climate Fund — established to channel climate finance to developing countries
5. Loss and Damage — discussions on compensation for irreversible climate damage (established at COP27 in 2022)

Q20. Evaluate the effectiveness of Ethiopia’s Green Legacy Initiative as a climate change strategy, considering both its potential benefits and possible limitations.

Answer:
Potential benefits:
Mitigation: Trees absorb $\text{CO}_2$, directly reducing atmospheric GHG concentrations
Adaptation: Trees regulate local water cycles, prevent soil erosion, provide shade, and support biodiversity
Economic: Forests provide timber, non-timber products, and employment opportunities
Social: The initiative mobilizes millions of citizens, raising climate awareness
Scale: Planting billions of seedlings creates a significant potential carbon sink
Alignment with CRGE: Directly supports Pillar 2 (protecting and restoring forests)

Possible limitations:
Survival rate: Not all planted seedlings survive to become mature trees. If survival rates are low, the actual carbon sequestration will be much less than the number planted suggests
Time lag: Trees take decades to sequester significant amounts of carbon — this does not solve the immediate problem
Tree species selection: If monocultures or non-native species are planted, biodiversity benefits may be limited and ecosystems could be disrupted
Land use conflicts: Tree planting on agricultural land could reduce food production, creating trade-offs
Maintenance: Long-term care of planted trees requires resources that may not be available
Verification: Accurately measuring the carbon sequestered is technically challenging

Conclusion: The Green Legacy Initiative is a valuable and ambitious strategy that aligns well with Ethiopia’s CRGE, but its effectiveness depends critically on seedling survival rates, appropriate species selection, long-term maintenance, and integration with broader land-use planning. It should complement, not replace, other mitigation and adaptation strategies.
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