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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?
Explanation
All three statements are correct.
**Statement I is correct:** In the absence of naturally occurring greenhouse effect, the average temperature of the earth surface would be -19°C instead of present value of 15°C and the earth would be a frozen lifeless planet.[1] Without greenhouse gases, the surface temperature of the planet would be about –19°C, and the Earth could not support life.[2] This demonstrates that temperatures would indeed be well below freezing everywhere without the atmosphere.
**Statement II is correct:** The greenhouse effect is a naturally occurring phenomenon that blankets the earth's lower atmosphere and warms it, maintaining the temperature suitable for living things to survive.[1] Greenhouse gases in the atmosphere absorb much of the infrared energy emitted from the Earth's surface, preventing it from escaping from the Earth's system. The greenhouse gases then re-emit this energy in all directions, warming the Earth's surface and lower atmosphere.[3]
**Statement III is correct:** Carbon dioxide is meteorologically a very important gas as it is transparent to the incoming solar radiation but opaque to the outgoing terrestrial radiation. It absorbs a part of terrestrial radiation and reflects back some part of it towards the earth's surface. It is largely responsible for the green house effect.[4]
Sources- [1] Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 17: Climate Change > 17.2. GREENHOUSE EFFECT > p. 254
- [2] Environment and Ecology, Majid Hussain (Access publishing 3rd ed.) > Chapter 6: Environmental Degradation and Management > Greenhouse Effect and Global Warming > p. 7
- [3] Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 17: Climate Change > Role of Greenhouse Gases > p. 255
- [4] FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 7: Composition and Structure of Atmosphere > Gases > p. 64
PROVENANCE & STUDY PATTERN
Guest previewThis is a classic 'First Principles' question bridging Physical Geography and Environment. It rewards conceptual clarity over rote memorization. If you understood the *physics* of the Heat Budget in NCERT Class XI, this was a free hit. Do not skip the introductory 'mechanism' paragraphs in standard texts.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Would Earth's surface temperatures be well below the freezing point everywhere on the planet if Earth had no atmosphere?
- Statement 2: Does heat absorbed and trapped by Earth's atmosphere (the greenhouse effect) maintain the planet's average surface temperature?
- Statement 3: Are atmospheric gases such as carbon dioxide particularly effective at absorbing and trapping Earth's outgoing infrared radiation?
- Gives a real example of a body with no atmosphere (the Moon) and reports its average surface temperature is below freezing.
- Supports the idea that a surface without an atmosphere can have a mean temperature well below 0°C.
- Quantifies the effect of removing a major greenhouse gas (CO2) on Earth's surface temperature: a drop of approximately 33°C.
- Together with Earth's current average (given in other passages), a ~33°C drop implies mean temperatures would fall well below the freezing point.
- States Earth's natural greenhouse effect maintains an average temperature of 15 °C (59 °F).
- Provides the baseline temperature which, when reduced by the ~33°C collapse noted above, indicates averages below freezing.
States that the atmosphere keeps surface temperature within certain limits and that in its absence extremes of temperature would exist between day and night.
A student could combine this with the idea of day–night radiative heating to infer that, without an atmosphere, nights could become much colder (possibly below freezing) while days could be much hotter.
Explains the planetary heat budget and that some incoming solar energy is reflected/absorbed by the atmosphere before reaching the surface.
One could extend this by estimating the surface energy that would remain without atmospheric reflection/absorption to judge how much solar heating the bare surface would receive and whether average temperatures might remain above or fall below freezing.
Notes that a moderate temperature on Earth arises partly because the planet is the right size to support an atmosphere, which plays a major role in sustaining life.
A student could infer that losing the atmosphere would remove that moderating influence and then compare Earth’s solar input (using a basic Sun–Earth distance map) to evaluate likely surface temperatures without atmospheric effects.
Provides examples of planets with listed average temperatures and whether they have atmospheres, implying a connection between atmosphere presence and planetary surface temperature.
By comparing the table’s temperatures and atmosphere presence, a student could use planetary examples (and their distances from the Sun) to reason whether an airless Earth would resemble the temperature extremes of other airless or thin-atmosphere bodies.
Describes that the atmosphere causes temperature to decrease with altitude because the atmosphere is heated from the surface (normal lapse rate).
A student could use this rule to argue that, without an atmosphere heated from the surface, the vertical temperature structure would change and surface heat retention (especially at night) would be reduced, affecting whether surfaces stay above freezing.
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