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Q51 (CDS-I/2006) Geography › World Physical Geography › Atmosphere composition Answer Verified

Assertion (A): The amount of dust particles is less in subtropical and temperate areas than in equatorial area. Reason (R): The atmosphere is dry and windy in the subtropical and temperate areas.

Result
Your answer: —  Â·  Correct: D
Explanation

The Assertion (A) is false because the concentration of dust particles is actually higher in subtropical and temperate regions compared to equatorial and polar regions [c1, t1]. This is primarily due to the presence of dry winds and arid conditions in these latitudes [c1]. The Reason (R) is true; subtropical and temperate areas, particularly those housing major hot deserts like the Sahara, are characterized by dry and windy conditions [c4, c5]. These dry winds facilitate the uplift and transport of fine soil and dust particles into the atmosphere [c2, t6]. In contrast, the equatorial region experiences high humidity and frequent rainfall, which leads to 'rain wash out' or wet deposition, effectively removing dust from the atmosphere [t2, t3]. Therefore, while the reason correctly describes the atmospheric conditions of these regions, the assertion incorrectly states the relative dust distribution.

Sources

  1. [1] FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 7: Composition and Structure of Atmosphere > Dust Particles > p. 65
  2. [2] FUNDAMENTALS OF PHYSICAL GEOGRAPHY, Geography Class XI (NCERT 2025 ed.) > Chapter 11: World Climate and Climate Change > Subtropical Steppe (BSh) and Subtropical Desert (BWh) Climates > p. 93
  3. [3] Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 14: Climate > Pressure and Planetary Winds > p. 140
  4. [4] Certificate Physical and Human Geography , GC Leong (Oxford University press 3rd ed.) > Chapter 7: Arid or Desert Landforms > Landforms of Wind Deposition in Deserts > p. 72
  5. [5] https://www.sciencedirect.com/topics/computer-science/atmospheric-condition
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