Climate Change: Natural and Man-made Causes, Changes in India and Adaptation, ISC Class 11
Updated 15 October 2026 · Fact-checked
Climate change is a long-term shift in average temperature and rainfall patterns. Natural causes include changes in solar output, the earth's orbit, volcanic eruptions and ocean circulation; recent warming is mainly man-made, from greenhouse gases released by burning fossil fuels and clearing forests. India faces more heatwaves, erratic monsoons and retreating glaciers, prompting adaptation.
What Climate Change is about
Weather is the state of the atmosphere over hours or days; climate is the average weather of a place over a long period, usually 30 years or more. Climate has always changed, but the warming of the last century has been unusually rapid.
The syllabus covers:
1. Causes of climatic change in the recent past: natural factors and man-made factors.
2. Climatic changes in India: rising temperatures, heatwaves, changes in monsoon rainfall, extreme rain, glacier retreat and sea-level rise.
3. Measures to adapt to these changes in urban and rural India.
4. Practical work: measuring rainfall with a rain gauge and drawing bar graphs of rainfall variation for Indian cities.
Mitigation means reducing the causes (cutting greenhouse-gas emissions); adaptation means adjusting to changes that are already happening. The syllabus stresses adaptation.
Weightage: CISCE gives no Class XI unit weightage for ISC Geography. Climate Change is topic 16 of the Class XI syllabus (Atmosphere) and can be asked anywhere in the 70-mark Paper I (Theory, 3 hours). Class XI is examined by the school, so your school sets the paper and decides how many marks each topic carries.Source: CISCE ISC Geography (853) syllabus, examination year 2028, Class XI
Key concepts
- Natural causes of climatic change
1. Changes in solar output: the energy given out by the sun varies slightly, for example with the roughly 11-year sunspot cycle. Long periods of very few sunspots have coincided with cooler periods.
2. Changes in the earth's orbit and tilt (Milankovitch cycles): slow, regular changes in the shape of the earth's orbit (eccentricity), the tilt of its axis (obliquity) and the wobble of the axis (precession) alter how much sunlight reaches different latitudes in different seasons. They pace the advance and retreat of ice ages over tens of thousands of years.
3. Volcanic eruptions: large explosive eruptions throw sulphur dioxide high into the stratosphere, forming sulphate aerosols that reflect sunlight and cool the earth for a year or two. The eruption of Mount Pinatubo (Philippines) in 1991 cooled global temperatures for about two years.
4. Ocean circulation and El Nino: shifts in ocean currents redistribute heat; El Nino years tend to be warmer globally, La Nina years cooler.
5. Movement of continents and changes in mountains (over millions of years) alter ocean currents and winds.
6. Changes in the earth's surface: more snow and ice reflect more sunlight (higher albedo), cooling further; melting reduces albedo and adds warming (feedback).These factors explain past ice ages and warm periods, but natural factors alone cannot explain the rapid warming since the mid-twentieth century.
Worked example
[4] Explain any four natural causes of climatic change. (Recall)
Try it first, then show the solutionSolution
- Variation in solar output (sunspot cycles) - 1 mark.
- Milankovitch cycles: orbit, tilt, wobble - 1 mark.
- Volcanic aerosols reflect sunlight and cool the earth - 1 mark.
- Ocean circulation changes (El Nino) or albedo feedback - 1 mark.
Answer: The sun's energy output varies slightly with sunspot activity; slow changes in the earth's orbit, tilt and wobble (Milankovitch cycles) change the distribution of sunlight and pace ice ages; large volcanic eruptions put sulphate aerosols into the stratosphere, reflecting sunlight and cooling the earth for a year or two; and changes in ocean circulation, such as El Nino, redistribute heat around the globe.
- Man-made causes and the enhanced greenhouse effect
The greenhouse effect is natural: water vapour, carbon dioxide and other gases let sunlight in but absorb outgoing long-wave radiation, keeping the earth about 33 degrees C warmer than it would otherwise be. Human activities have increased these gases, strengthening the effect (the enhanced greenhouse effect) and causing global warming.
Man-made factors
1. Burning fossil fuels (coal, oil, natural gas) for electricity, industry and transport: the main source of carbon dioxide; atmospheric CO2 has risen from about 280 parts per million before the Industrial Revolution to over 400 ppm today.
2. Deforestation and land-use change: fewer trees to absorb CO2; burning forests releases carbon.
3. Agriculture: methane from flooded rice fields and cattle; nitrous oxide from nitrogen fertilisers.
4. Industry and waste: methane from landfills; CFCs and HFCs (also powerful greenhouse gases); cement production releases CO2.
5. Urbanisation: concrete and asphalt absorb heat, creating urban heat islands; vehicles and air-conditioners add heat.
6. Aerosols from pollution: some (sulphates) cool by reflecting sunlight, while black carbon (soot) warms and darkens snow and ice, speeding melting.The main greenhouse gases are carbon dioxide, methane, nitrous oxide, CFCs and HFCs, and water vapour (which increases as the air warms, amplifying warming).
Worked example
[4] Explain how human activities are causing global warming. (Understanding)
Try it first, then show the solutionSolution
- Burning fossil fuels releases CO2 - 1 mark.
- Deforestation reduces absorption and releases carbon - 1 mark.
- Agriculture and waste add methane and nitrous oxide - 1 mark.
- More greenhouse gases trap more outgoing heat: enhanced greenhouse effect - 1 mark.
Answer: Burning coal, oil and gas releases carbon dioxide; cutting and burning forests both releases carbon and removes trees that absorb it; rice paddies, cattle, fertilisers and landfills add methane and nitrous oxide. These greenhouse gases absorb more of the long-wave radiation leaving the earth, strengthening the natural greenhouse effect and raising global temperatures.
- Climatic changes in India
Observed and expected changes (based on India's own climate assessments)
1. Rising temperatures: India's average temperature rose by about 0.7 degrees C between 1901 and 2018, with more warm days and nights.
2. Heatwaves: more frequent, longer and more intense heatwaves in northern, central and eastern India, raising deaths from heatstroke and stress on power and water supply.
3. Monsoon rainfall: summer monsoon rainfall has become more erratic, with a decline over some regions such as the Indo-Gangetic plains in recent decades, longer dry spells and more frequent extreme rainfall events (very heavy rain on a single day), causing urban floods as in Mumbai and Chennai.
4. Droughts and floods: more frequent droughts in some regions and more intense floods in others.
5. Himalayan glaciers: many are retreating and thinning, threatening river flows in the long term and increasing risk of glacial lake outburst floods.
6. Sea-level rise and cyclones: rising seas threaten low coasts such as the Sundarbans; very severe cyclones over the Arabian Sea have become more frequent.
7. Effects: lower crop yields under heat stress, water scarcity, spread of vector-borne diseases, loss of biodiversity and damage to coastal livelihoods.Worked example
[4] Describe four effects of climate change already observed in India. (Understanding)
Try it first, then show the solutionSolution
- Rise in average temperature (about 0.7 degrees C, 1901-2018) - 1 mark.
- More frequent and intense heatwaves - 1 mark.
- Erratic monsoon, more extreme rainfall and floods - 1 mark.
- Glacier retreat or sea-level rise threatening coasts - 1 mark.
Answer: India's average temperature has risen by about 0.7 degrees C since 1901; heatwaves have become more frequent and intense; the monsoon has become more erratic, with longer dry spells and more days of extreme rain causing floods; and Himalayan glaciers are retreating while rising seas and stronger cyclones threaten low-lying coasts such as the Sundarbans.
- Adaptation in urban India
Cities concentrate people, heat and paved surfaces, so they face heatwaves, waterlogging and water shortages.
Measures
1. Heat action plans: early warnings, cooling centres, drinking-water points, changed working hours for outdoor workers and preparation of hospitals. Ahmedabad's Heat Action Plan (2013) was the first of its kind in South Asia and has been copied by many cities.
2. Cool roofs and green cover: reflective white roofs, rooftop gardens, urban forests and parks reduce indoor and outdoor temperatures and the urban heat island.
3. Water management: compulsory rainwater harvesting on buildings, recharge of groundwater, revival of lakes and tanks, reuse of treated wastewater.
4. Flood management: better storm-water drains, keeping natural drainage channels and wetlands free of encroachment, flood warning systems.
5. Climate-smart buildings and planning: energy-efficient design, natural ventilation, building codes, protection of mangroves along coastal cities.
6. Public transport and clean energy also cut emissions (mitigation) while reducing heat and pollution.India's National Action Plan on Climate Change (2008) set up national missions, including one on sustainable habitat, that guide such work.
Worked example
[4] Suggest four measures Indian cities can take to adapt to more frequent heatwaves and extreme rainfall. (Evaluate)
Try it first, then show the solutionSolution
- Heat action plans with early warnings and cooling centres - 1 mark.
- Cool roofs, trees and parks to reduce the heat island - 1 mark.
- Storm-water drains; protect wetlands and drainage channels - 1 mark.
- Rainwater harvesting and groundwater recharge - 1 mark.
Answer: Cities can adopt heat action plans with early warnings, cooling centres and drinking-water points; use cool roofs, trees and parks to reduce the urban heat island; improve storm-water drainage and keep wetlands and natural channels free so heavy rain drains away; and make rainwater harvesting compulsory to recharge groundwater for dry spells.
- Adaptation in rural India and practical work on rainfall
Rural adaptation (farming depends directly on climate)
1. Water conservation: watershed development, check dams, farm ponds, revival of traditional tanks and johads, and water-conservation works under rural employment schemes.
2. Efficient irrigation: drip and sprinkler irrigation to grow more crop per drop.
3. Climate-resilient crops: drought-, flood- and heat-tolerant varieties, changing sowing dates, crop diversification (millets, pulses) and mixed cropping.
4. Risk protection: crop insurance (such as the Pradhan Mantri Fasal Bima Yojana, 2016), weather-based advisories to farmers by mobile phone, and soil health cards.
5. Agroforestry and soil conservation: trees on farms, mulching and contour bunding protect soil and moisture.
6. Livelihood diversification: dairying, poultry and non-farm work to spread risk.Practical work: measuring rainfall
1. A rain gauge is a cylindrical container with a funnel of known diameter leading into a collecting bottle. It is placed in an open space, away from trees and buildings, with its rim about 30 cm above the ground.
2. Each day at a fixed time, the collected water is poured into a measuring cylinder graduated in millimetres of rainfall.
3. Rainfall is expressed as the depth of water in mm that would cover a flat surface.
4. Bar graph: draw months on the x-axis and rainfall (mm) on the y-axis, with bars of equal width and gaps; give a title, scale and key. Comparing two cities' bars shows differences in monsoon pattern (for example a city with a single summer peak against one with rain in October-December).
5. Departure from normal (%) = (actual - normal) / normal x 100.Worked example
[4] Explain how rainfall is measured with a rain gauge and how a bar graph of monthly rainfall is drawn. (Application)
Try it first, then show the solutionSolution
- Rain gauge: funnel and collecting bottle in an open place, rim about 30 cm above ground - 1 mark.
- Water measured daily at a fixed time in a cylinder graduated in mm - 1 mark.
- Bar graph: months on x-axis, rainfall (mm) on y-axis, equal bars - 1 mark.
- Title, scale and key; compare peaks between cities - 1 mark.
Answer: A rain gauge, a funnel leading into a collecting bottle, is set in an open place with its rim about 30 cm above the ground; each day at a fixed time the water is poured into a measuring cylinder graduated in millimetres. For a bar graph, months are marked on the x-axis and rainfall in mm on the y-axis, with bars of equal width, a title, a scale and a key.
Climate Change in real life
Each concept, met in an everyday situation. Read the situation, answer the question in your own words, then compare with the model answer. The one-line hook is what to remember.
Greenhouse effect
Suppose a car is parked in the sun with its windows shut; after an hour the inside is far hotter than the air outside.
How does this model the greenhouse effect, and what does adding more greenhouse gases do?
Try it first, then show the solutionSolution
- Sunlight passes through the glass and heats the seats.
- The heat given off cannot easily escape through the glass.
- Greenhouse gases act like the glass; more gases trap more heat.
Answer: The car models the greenhouse effect: sunlight enters but the heat cannot easily escape. Greenhouse gases play the role of the glass, so increasing them traps more outgoing heat and warms the earth.
Memory hook: More glass, more heat.
Rainfall departure
Imagine a district's normal June-September rainfall is 800 mm, but this year it receives 620 mm.
Calculate the departure from normal and suggest one adaptation for farmers.
Try it first, then show the solutionSolution
- Departure = (620 - 800) / 800 x 100.
- = -180 / 800 x 100 = -22.5 per cent.
- A deficit of this size calls for drought-tolerant crops or farm ponds.
Answer: The departure is -22.5 per cent (a deficit); farmers can adapt with farm ponds to store water, drip irrigation and drought-tolerant crops such as millets.
Memory hook: Measure the shortfall, plan the crop.
Urban heat island
Suppose at night you walk from a tree-lined park to a crowded market with concrete and asphalt; the market feels several degrees warmer.
Why, and how can cities reduce this effect?
Try it first, then show the solutionSolution
- Concrete and asphalt absorb heat by day and release it at night.
- Few trees mean little shade or cooling by evaporation.
- Cool roofs, trees and parks reduce the heat island.
Answer: The market is an urban heat island: paved surfaces store and release heat, and there is little vegetation. Trees, parks, water bodies and reflective cool roofs reduce it.
Memory hook: Concrete keeps the heat; trees give it back.
Topics in this chapter
Climate Change: key facts
- Natural causes
- Solar output, Milankovitch cycles, volcanoes, ocean circulation, albedo feedback
- Pinatubo 1991 cooled the earth.
- Man-made causes
- Fossil fuels, deforestation, agriculture, industry/waste, urbanisation
- CO2 280 ppm -> over 400 ppm.
- Changes in India
- +0.7 degrees C (1901-2018), heatwaves, erratic monsoon, extreme rain, glacier retreat, sea-level rise
- Climate assessment for the Indian region.
- Adaptation
- Urban: heat action plans, cool roofs, drains, rainwater harvesting; rural: watersheds, drip irrigation, resilient crops, insurance
- NAPCC 2008.
- Rainfall departure
- 620 vs 800 mm = -22.5%.
- Mean monthly rainfall
- For bar graphs.
How the school exam asks Climate Change
The question patterns to expect, and the method that works for each.
| Question type | How it is asked | Method |
|---|---|---|
| Causes | Natural and man-made causes of climatic change; greenhouse effect. | Mechanism for each cause, with an example. |
| India and adaptation | Effects of climate change in India; adaptation measures in urban and rural areas. | Effect -> measure pairs with Indian examples. |
| Practical | Use of rain gauge; draw and interpret rainfall bar graphs; calculate totals, means and departures. | Method steps, then full working. |
Tricks to remember Climate Change
Short memory aids. Say each one aloud once, then use it on a question the same day.
Natural causes: 'SOVO'
Sun, Orbit, Volcanoes, Oceans.
Use it when: Natural factors.
Man-made: 'FDAIU'
Fuels, Deforestation, Agriculture, Industry, Urbanisation.
Use it when: Human factors.
Adapt versus mitigate
Mitigation Minimises the cause; Adaptation Adjusts to the effect.
Use it when: Avoid mixing the two.
Climate Change: exam-level solved questions
Ordered from exam level to HOTS. Cover the solution, write your own, then compare step by step.
Example 1: Volcanic cooling · 1 mark · MCQExam level
Large volcanic eruptions tend to cool the earth for a year or two because they:
(a) Release carbon dioxide
(b) Put sulphate aerosols into the stratosphere that reflect sunlight
(c) Melt glaciers
(d) Increase solar output
Try it first, then show the solutionSolution
- Sulphur dioxide forms reflective sulphate aerosols high up.
- Less sunlight reaches the surface.
Answer: (b) Put sulphate aerosols into the stratosphere that reflect sunlight.
Example 2: Assertion-reason: recent warming · 1 mark · Assertion-reasonHarder exam level
Assertion (A): The warming of the last several decades is mainly due to human activities.
Reason (R): Natural factors such as the sun and volcanoes cannot account for the rapid rise in temperature, which matches the rise in greenhouse gases.
(a) Both A and R are true and R is the correct explanation of A.
(b) Both A and R are true but R is not the correct explanation of A.
(c) A is true but R is false.
(d) A is false but R is true.
Try it first, then show the solutionSolution
- Solar output has not risen enough to explain the warming.
- Greenhouse gases from fuels and land use match the trend, so R explains A.
Answer: (a) Both A and R are true and R is the correct explanation of A.
Example 3: Rainfall table · 4 marks · Short answerHarder exam level
[4] Suppose a city records monthly rainfall (mm): Jan 10, Feb 15, Mar 20, Apr 25, May 40, Jun 180, Jul 320, Aug 300, Sep 190, Oct 60, Nov 20, Dec 10. Find the annual total, the share of June-September in it, and the mean monthly rainfall. What does the bar graph show? (Application)
Try it first, then show the solutionSolution
- Annual total = 1,190 mm.
- June-September = 180 + 320 + 300 + 190 = 990 mm = 990 / 1,190 x 100 = about 83.2 per cent.
- Mean monthly = 1,190 / 12 = about 99.2 mm.
- The graph shows a sharp single peak in July-August: rain from the south-west monsoon.
Answer: Annual total = 1,190 mm. June-September = 990 mm, about 83 per cent of the year's rain. Mean monthly rainfall = 1,190/12 = about 99.2 mm. The bar graph would show low bars for most of the year and a sharp peak in July-August, typical of a city dependent on the south-west monsoon.
Example 4: Monsoon and agriculture · 4 marks · Short answerHOTS / competency
[4] Why does a change in monsoon rainfall pattern threaten Indian agriculture more than a small rise in average temperature? (Analysis)
Try it first, then show the solutionSolution
- Much farmland is rainfed and depends on monsoon timing.
- Delayed onset or long dry spells hit sowing and germination.
- Extreme rainfall floods fields and erodes soil.
- Small average warming matters less than the timing and spread of rain, though heat stress at flowering also lowers yields.
Answer: A large share of Indian farmland is rainfed, so crops depend on the timing and spread of monsoon rain. A late onset or long dry spells disrupt sowing and growth, while extreme downpours flood fields and wash away soil. A small rise in the average temperature matters less than such changes in rain, although heat stress at flowering time also reduces yields.
Example 5: Climate change and India · 7 marks · Long answerHarder exam level
[7] (a) Explain the natural and man-made causes of climatic change. [4]
(b) Describe three measures to adapt to climate change in rural India. [3] (Understanding)
Try it first, then show the solutionSolution
- (a) Natural: solar output and Milankovitch cycles (1).
- (a) Natural: volcanic aerosols, ocean circulation (1).
- (a) Man-made: fossil fuels releasing CO2; deforestation (1).
- (a) Man-made: methane, nitrous oxide; enhanced greenhouse effect (1).
- (b) Watershed development, farm ponds, check dams (1).
- (b) Drip and sprinkler irrigation; resilient crop varieties (1).
- (b) Crop insurance and weather advisories; agroforestry (1).
Answer: (a) Natural causes include changes in the sun's output, slow changes in the earth's orbit and tilt (Milankovitch cycles), volcanic eruptions whose aerosols reflect sunlight, and changes in ocean circulation such as El Nino. Man-made causes include burning fossil fuels and clearing forests, which raise carbon dioxide, and agriculture and waste, which add methane and nitrous oxide; these strengthen the greenhouse effect and warm the earth. (b) Rural India can adapt through watershed development, farm ponds and check dams to store water; drip and sprinkler irrigation and drought- or flood-tolerant crop varieties; and crop insurance and weather-based advisories to protect farmers from losses.
Example 6: Two cities compared · 4 marks · Short answerHarder exam level
[4] Suppose City A gets 75 per cent of its annual rain from June to September, while City B gets 50 per cent of its rain from October to December. Suggest which coasts of India the cities may lie on and explain why. (Evaluate)
Try it first, then show the solutionSolution
- City A: summer peak typical of the south-west monsoon (west coast or most of India).
- City B: autumn-winter peak typical of the Tamil Nadu (Coromandel) coast.
- Tamil Nadu lies in the rain shadow of the Western Ghats in summer.
- It gets rain from the retreating (north-east) monsoon and cyclones in October-December.
Answer: City A, with most rain in June-September, is likely on the west coast or elsewhere in monsoon India, watered by the south-west monsoon. City B, with half its rain in October-December, is likely on the Tamil Nadu (Coromandel) coast, which lies in the rain shadow of the Western Ghats in summer and receives rain from the retreating north-east monsoon and Bay of Bengal cyclones.
Case-study practice (Section D style)
Read the situation, then answer every part. In a school exam set on the board pattern this is a 8-mark question split into 2 + 2 + 2 + 2 marks.
A village adapts (source-based)
Read the imaginary account and answer.
'Ten years ago our village depended on one crop of paddy. The monsoon now arrives late, and dry spells of three weeks are common, but some days bring very heavy rain. The panchayat dug farm ponds and check dams; farmers switched part of their land to millets and pulses and installed drip irrigation for vegetables. Many joined a crop insurance scheme and receive weather messages on their phones.'
(i) · 2 marks
Identify two signs of climate change described in the account.
Answer
Answer: Late monsoon onset with long dry spells; very heavy rain on some days (extreme rainfall).
1 mark each.
(ii) · 2 marks
How do farm ponds and check dams help in both dry spells and heavy rain?
Answer
Answer: They capture runoff during heavy rain, reducing floods and erosion, and store water for irrigation and groundwater recharge during dry spells.
1 for each situation.
(iii) · 2 marks
Why is switching to millets and pulses a sensible adaptation?
Answer
Answer: They need much less water than paddy and tolerate heat and dry spells better, so they reduce the risk of crop failure.
1 for water need; 1 for tolerance.
(iv) · 2 marks
Is the crop insurance scheme adaptation or mitigation? Explain.
Answer
Answer: Adaptation: it does not reduce greenhouse gases but helps farmers cope with losses from climate-related events.
1 for answer; 1 for reason.
Where the marks are
How a typical answer is split into step marks. Show every step: a right final answer alone rarely earns full marks.
[4] Man-made causes of climate change. (4 marks)
| Step | Marks |
|---|---|
| Fossil fuels and CO2. | 1 |
| Deforestation and land use. | 1 |
| Agriculture and waste: methane, nitrous oxide. | 1 |
| Enhanced greenhouse effect explained. | 1 |
[7] Climate change in India and adaptation. (7 marks)
| Step | Marks |
|---|---|
| Temperature rise and heatwaves. | 1 |
| Erratic monsoon and extreme rain. | 1 |
| Glaciers, sea level or cyclones. | 1 |
| Urban: heat action plans, cool roofs. | 1 |
| Urban: drains, rainwater harvesting. | 1 |
| Rural: water conservation, efficient irrigation. | 1 |
| Rural: resilient crops, insurance. | 1 |
Where students lose marks in Climate Change
The slips examiners see most often, and what to write instead.
Mistake: Confusing ozone depletion with global warming
Both are atmospheric problems.
Wrong working
The ozone hole causes global warming.
Right working
Global warming is caused by greenhouse gases; ozone depletion lets in more UV.
Do this: Keep the two causes and effects separate.
Usually costs: 1-2 marks.
Mistake: Listing mitigation when adaptation is asked
Terms mixed.
Do this: Adaptation = coping (drains, crops, heat plans); mitigation = cutting emissions.
Usually costs: 1-2 marks.
Mistake: Saying the greenhouse effect is entirely harmful
Natural effect forgotten.
Do this: It keeps the earth habitable; the problem is its enhancement.
Usually costs: 1 mark.
Mistake: Bar graph without scale or title
Presentation marks lost.
Do this: Label axes, give a scale, a title and a key.
Usually costs: 1 mark.
Mistake: No Indian reference
The syllabus asks for India.
Do this: Heatwaves, monsoon, glaciers, Ahmedabad plan, farm ponds, NAPCC.
Usually costs: 1 mark.
Practice questions on Climate Change
Write each answer on paper first. Open the hint only if you are stuck, and the answer only when you have finished.
Q1 · 1 mark · Very short answerExam level
Distinguish between weather and climate in one sentence.
Hint
Time span.
Answer
Weather is the short-term state of the atmosphere; climate is the average weather over a long period (about 30 years or more).
Q2 · 1 mark · Very short answerExam level
Name the main greenhouse gas released by burning fossil fuels.
Hint
CO2.
Answer
Carbon dioxide.
Q3 · 1 mark · MCQExam level
Methane is released in large amounts by:
(a) Wind turbines
(b) Flooded rice fields and cattle
(c) Solar panels
(d) Forests growingHint
Agriculture.
Answer
(b) Flooded rice fields and cattle.
Q4 · 1 mark · Very short answerHarder exam level
Which Indian city prepared South Asia's first heat action plan?
Hint
Gujarat, 2013.
Answer
Ahmedabad.
Q5 · 4 marks · Short answerHarder exam level
[4] Explain how Milankovitch cycles cause climatic change.
Hint
Orbit, tilt, wobble.
Answer
(1) The shape of the earth's orbit changes slowly between more circular and more elliptical (eccentricity). (2) The tilt of the axis varies slightly (obliquity). (3) The axis wobbles, changing the season when the earth is nearest the sun (precession). (4) Together they alter the amount of summer sunlight in high latitudes over tens of thousands of years, pacing ice ages.
Q6 · 4 marks · Short answerHarder exam level
[4] Why are Himalayan glaciers important, and how does climate change threaten them?
Hint
Rivers.
Answer
(1) They feed perennial rivers like the Ganga and Indus, especially in the dry pre-monsoon season. (2) Warming makes many of them retreat and thin. (3) Black carbon (soot) darkens the ice and speeds melting. (4) In the long term river flows may fall, while meltwater lakes dammed by moraines can burst and flood valleys.
Q7 · 4 marks · Short answerHarder exam level
[4] Explain why coastal cities like Mumbai are vulnerable to climate change, and suggest two adaptations.
Hint
Rain, sea.
Answer
(1) Extreme rainfall events overwhelm drains and flood low-lying areas. (2) Rising sea level and storm surges threaten reclaimed land and coastal settlements. (3) Adaptation: improve storm-water drains and keep natural channels and wetlands clear. (4) Protect and restore mangroves, which absorb surge energy, and set up flood warnings.
Q8 · 4 marks · Short answerHOTS / competency
[4] A city's normal annual rainfall is 1,500 mm. Over three years it receives 1,140 mm, 1,725 mm and 1,500 mm. Calculate the percentage departure for each year and the three-year average.
Hint
(actual - normal) / normal x 100.
Answer
(1) Year 1: (1,140 - 1,500)/1,500 x 100 = -24 per cent. (2) Year 2: (1,725 - 1,500)/1,500 x 100 = +15 per cent. (3) Year 3: 0 per cent. (4) Average = (1,140 + 1,725 + 1,500)/3 = 4,365/3 = 1,455 mm, which is 3 per cent below normal; the swings show increasing variability.
Q9 · 4 marks · Short answerHOTS / competency
[4] 'Adaptation is necessary even if all emissions stopped today.' Evaluate this statement.
Hint
Lag; long-lived gases.
Answer
(1) Carbon dioxide stays in the atmosphere for a very long time, so existing gases will keep warming the earth. (2) Oceans warm slowly and sea level will go on rising for decades. (3) Heatwaves, erratic monsoons and glacier retreat are already affecting India. (4) So the statement is valid: mitigation limits future change, but adaptation is needed to cope with changes already locked in.
Test your recall
Answer in your head or on paper first, then open the card. Pulling an answer out of memory makes it stick far better than re-reading.
1.What was the pre-industrial level of carbon dioxide?Show answer
About 280 parts per million.
2.Which eruption of 1991 cooled the earth?Show answer
Mount Pinatubo, Philippines.
3.When did India release its National Action Plan on Climate Change?Show answer
2008.
4.At what height is a rain gauge's rim usually kept?Show answer
About 30 cm above the ground.
5.What is an urban heat island?Show answer
A city area warmer than its surroundings because of paved surfaces, buildings and waste heat.
6.By about how much did India's average temperature rise from 1901 to 2018?Show answer
About 0.7 degrees C.
Best order to study it
- Weather, climate and the greenhouse effect.
- Natural causes.
- Man-made causes.
- Changes observed in India.
- Adaptation in towns and villages; rain gauge and bar graphs.
Quick revision checklist
The night before the exam: can you do each of these without looking?
- Climate = average weather over about 30 years; recent warming is rapid.
- Natural: sun, Milankovitch cycles, volcanoes (Pinatubo 1991), ocean circulation, albedo.
- Man-made: fossil fuels (CO2 280 -> 400+ ppm), deforestation, methane, nitrous oxide, HFCs, urban heat.
- India: +0.7 degrees C (1901-2018), heatwaves, erratic monsoon, extreme rain, glacier retreat, sea-level rise.
- Urban adaptation: heat action plans (Ahmedabad 2013), cool roofs, trees, drains, rainwater harvesting.
- Rural adaptation: watersheds, farm ponds, drip irrigation, resilient crops, insurance, advisories.
- Rain gauge: open site, rim ~30 cm; measure daily in mm; bar graph with title, scale, key.
- Departure (%) = (actual - normal)/normal x 100.
Climate Change: frequently asked questions
Is global warming the same as climate change?
Global warming is the rise in average global temperature; climate change is the wider set of changes it brings, including rainfall, storms and sea level.
Do I need to know international agreements?
The syllabus focuses on causes and adaptation in India. A brief mention of India's National Action Plan on Climate Change and of global efforts to cut emissions is enough.
Can I use real rainfall data of my city?
Yes. Use data recorded at your school or published by the weather service, and always state the source and period on your graph.
Based on: CISCE ISC 2028 Geography (853) syllabus (Classes XI and XII); CISCE Regulations for the ISC Examination Year 2028 (Class XI internal examination)