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UPSC Prelims 2025Question 29Geography

Consider the following statements:
I. Without the atmosphere, temperature would be well below freezing point everywhere on the
Earth's surface.
II. Heat absorbed and trapped by the atmosphere maintains our planet's average temperature.
III. Atmosphere's gases, like carbon dioxide, are particularly good at absorbing and trapping radiation.
Which of the statements given above are correct?

Options

  1. (a)I and III only
  2. (b)I and II only
  3. (c)I, II and III
  4. (d)II and III only
Correct answer: c
Decision rule

Statements tracing successive links of one accepted mechanism — gases absorb infrared, trapping sets mean temperature, absence means freezing — stand or fall together.

Explanation

Correct Answer:

(c) I, II and III


Explanation of the Correct Answer:

All three statements are correct and interrelated aspects of how the Earth's atmosphere regulates temperature:


Statement I: Without the atmosphere, temperature would be well below freezing point everywhere on the Earth's surface.

  • Correct.
  • The average surface temperature of Earth is about 15°C due to the greenhouse effect.
  • Without an atmosphere, Earth’s average temperature would fall to around 18°C, making life as we know it impossible.
  • The atmosphere traps heat and slows down the rate of heat loss to outer space.

Statement II: Heat absorbed and trapped by the atmosphere maintains our planet's average temperature.

  • Correct.
  • The greenhouse effect allows solar radiation to enter, but certain gases (like CO₂ and water vapor) trap the infrared radiation (heat) re-emitted by Earth’s surface.
  • This process stabilizes Earth’s climate and keeps it habitable.

Statement III: Atmosphere's gases, like carbon dioxide, are particularly good at absorbing and trapping radiation.

  • Correct.
  • Greenhouse gases such as carbon dioxide (CO₂), methane (CH₄), and water vapor (H₂O) absorb outgoing infrared radiation.
  • CO₂, in particular, is efficient at trapping longwave radiation, significantly contributing to warming.

Why Other Options Are Incorrect:

  • (a) I and III only: Excludes II, which is essential and correct.
  • (b) I and II only: Excludes III, which is scientifically validated.
  • (d) II and III only: Excludes I, which is fundamental to understanding the role of the atmosphere.

Relevant Supplementary Information

Table: Greenhouse Gases and Their Roles

GasAbundanceHeat Absorbing CapacitySources
Carbon dioxide (CO₂)ModerateHighFossil fuel burning, deforestation
Methane (CH₄)LowVery highLivestock, rice paddies, landfills
Water vapor (H₂O)HighModerate to highEvaporation, transpiration
Nitrous oxide (N₂O)Very lowHighAgriculture, fertilizers
Ozone (O₃)VariableModerateTroposphere (pollution), stratosphere (protective layer)

Table: Comparison – Earth with vs. without Atmosphere

FactorWith AtmosphereWithout Atmosphere
Average Surface Temperature~15°C~-18°C
Heat RetentionHigh (via greenhouse effect)Very low
Temperature FluctuationsModerateExtreme day-night differences
HabitabilityLife-supportingHostile

Related Concepts:

  • Greenhouse Effect: Natural process by which certain gases trap heat in Earth's atmosphere.
  • Infrared Radiation: Longwave radiation emitted by Earth after absorbing sunlight.
  • Earth's Energy Budget: Balance between incoming solar energy and outgoing infrared radiation.

Current Relevance:

  • Understanding the natural greenhouse effect is essential for analyzing climate change.
  • Rising levels of CO₂ and CH₄ due to human activity are intensifying the greenhouse effect, leading to global warming.
  • International efforts like the Paris Agreement focus on reducing greenhouse gas emissions.

Table 1: Role of the Atmosphere in Earth's Temperature Regulation

AspectWith AtmosphereWithout Atmosphere
Average Surface Temperature~15°C~-18°C
Heat RetentionEffective (via greenhouse gases)Minimal (heat quickly lost to space)
Temperature FluctuationModerate day-night variationExtreme variation between day and night
Condition for LifeSupports lifeHarsh, likely uninhabitable
Energy FlowIncoming solar radiation absorbed & re-radiatedNo insulation effect; high energy loss

Table 2: Greenhouse Effect – Natural vs. Enhanced

TypeCauseEffect
Natural Greenhouse EffectNaturally occurring greenhouse gasesKeeps Earth’s climate habitable
Enhanced Greenhouse EffectHuman-induced emissions from fossil fuels, etc.Leads to global warming and climate disruption

Table 3: Key Greenhouse Gases and Their Characteristics

GasChemical FormulaRelative AbundanceGlobal Warming Potential (GWP)Key Sources
Carbon DioxideCO₂High1Fossil fuels, deforestation
MethaneCH₄Low~28–34 (over 100 years)Cattle, rice paddies, landfills
Nitrous OxideN₂OVery Low~298Fertilizers, biomass burning
Water VapourH₂OVariable (Highest naturally)N/A (feedback gas)Evaporation, transpiration
Ozone (Tropospheric)O₃VariableModeratePhotochemical smog (pollution byproduct)

Table 4: Heat Transfer and Atmospheric Interaction

ProcessDescription
InsolationIncoming solar radiation absorbed by Earth’s surface
Terrestrial RadiationLongwave radiation re-emitted by Earth
Absorption by GHGsGreenhouse gases absorb infrared radiation and re-radiate it toward Earth
Temperature RegulationMaintains global temperature balance and supports ecosystems

Table 5: Statement-Based Concept Mapping

StatementAssociated ConceptScientific Justification
Statement IAtmosphere's Role in InsulationPrevents surface from freezing by retaining heat
Statement IIGreenhouse EffectAtmospheric gases trap re-radiated heat to regulate temperature
Statement IIIRole of CO₂ and GHGsCarbon dioxide efficiently absorbs infrared radiation

Extension: Atmospheric Composition (By Volume)

GasApproximate % in Atmosphere
Nitrogen (N₂)78.08%
Oxygen (O₂)20.95%
Argon (Ar)0.93%
Carbon Dioxide (CO₂)~0.04%
Water Vapor (H₂O)Variable (0–4%)


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