Question map
Consider the following statements : Statement-I : The atmosphere is heated more by incoming solar radiation than by terrestrial radiation. Statement-II : Carbon dioxide and other greenhouse gases in the atmosphere are good absorbers of long wave radiation. Which one of the following is correct in respect of the above statements ?
Explanation
The correct answer is option D because Statement-I is incorrect while Statement-II is correct.
The bulk of the incoming solar radiation is absorbed by the Earth's surface, not[1] by the atmosphere[2]. The atmosphere transmits the incoming solar radiation but absorbs the vast majority of long wave radiation emitted upwards by the earth's surface[3]. This means the atmosphere is heated MORE by terrestrial (longwave) radiation than by incoming solar radiation, making Statement-I incorrect.
Statement-II is correct because carbon dioxide is transparent to the incoming solar radiation but opaque to the outgoing terrestrial radiation, and it absorbs a part of terrestrial radiation and reflects back some part of it towards the earth's surface[4]. Greenhouse gases in the atmosphere absorb much of the infrared energy emitted from the Earth's surface, preventing it from escaping, and then re-emit this energy in all directions, warming the Earth's surface and lower atmosphere[5].
Therefore, Statement-I is incorrect but Statement-II is correct, making option D the right answer.
Sources- [1] https://www.ipcc.ch/site/assets/uploads/2018/02/ar4-wg1-faqs-1.pdf
- [2] https://www.ipcc.ch/site/assets/uploads/2018/03/ipcc_far_wg_I_full_report.pdf
- [3] FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 11: World Climate and Climate Change > Global Warming > p. 96
- [4] FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 7: Composition and Structure of Atmosphere > Gases > p. 64
- [5] Environment, Shankar IAS Acedemy .(ed 10th) > Chapter 17: Climate Change > Role of Greenhouse Gases > p. 255
PROVENANCE & STUDY PATTERN
Guest previewThis is a classic 'First Principles' Geography question directly from NCERT Class XI. It tests the fundamental physics of the Greenhouse Effect (Shortwave In vs. Longwave Out). If you understand why temperature decreases with height (Lapse Rate), you know the heat source is the ground, not the sun directly.
This question can be broken into the following sub-statements. Tap a statement sentence to jump into its detailed analysis.
- Statement 1: Is Earth's atmosphere heated more by incoming solar (shortwave) radiation than by terrestrial (longwave) radiation?
- Statement 2: Do carbon dioxide and other greenhouse gases in Earth's atmosphere strongly absorb longwave (thermal infrared) radiation?
- Statement 3: Does absorption of longwave radiation by carbon dioxide and other greenhouse gases explain why Earth's atmosphere is heated more by incoming solar radiation than by terrestrial radiation?
- Provides an energy-budget style breakdown with magnitudes showing atmospheric absorption of solar vs. large longwave exchanges (e.g., back radiation).
- Shows back radiation (~390 W/m2) and surface longwave fluxes are large compared with direct atmospheric solar absorption values in the same budget.
- States that about half of incoming solar is absorbed by the surface rather than directly by the atmosphere.
- Explains that the atmosphere is heated by energy transferred from the surface (thermals, evapotranspiration) and by longwave radiation absorbed by clouds and greenhouse gases.
- Explicitly states that the bulk of incoming solar radiation is absorbed by the Earth's surface, not the atmosphere.
- Implies the atmosphere's heating is largely driven by surface-absorbed solar energy being redistributed rather than direct shortwave absorption by the atmosphere.
States the atmosphere is largely transparent to incoming shortwave solar radiation, with most solar reaching the surface (some near‑IR/water vapour absorption and scattering occur).
A student could combine this with the fact that if most shortwave reaches the surface, then direct atmospheric heating from shortwave is limited compared to surface absorption.
Explains that the warmed Earth radiates longwave energy upward and that this terrestrial longwave is absorbed by greenhouse gases, heating the atmosphere from below.
Combine with estimates of surface emission (from surface temperature) to infer the magnitude of longwave energy available to heat the atmosphere.
Gives the general rule: atmosphere is mostly transparent to incoming shortwave but actively absorbs outgoing terrestrial longwave; links this to temperature lapse rate.
Use this rule plus the vertical distribution of greenhouse gases (concentrated near surface) to argue that absorbed longwave dominates near‑surface atmospheric heating.
Summarises the greenhouse effect: atmosphere transmits incoming solar but absorbs the vast majority of longwave emitted by the surface.
A student could take this qualitative ‘vast majority’ claim and compare it to known solar fluxes (insolation) to judge which flux heats the atmosphere more.
Shows an important exception: high-altitude thermosphere absorbs shortwave solar radiation strongly, producing high temperatures aloft.
Combine this with knowledge of atmospheric mass/energy distribution to note that shortwave heating can dominate in upper layers while longwave heating dominates the lower atmosphere.
This statement analysis shows book citations, web sources and indirect clues. The first statement (S1) is open for preview.
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