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Which of the following is true about the inversion ?
Question

Which of the following is true about the inversion ?

A.

Temperature of Earth’s surface is less than high altitudes in the atmosphere

B.

Temperature of Earth’s surface and high altitude atmosphere is same

C.

Temperature of Earth’s surface is more than high altitudes in the atmosphere

D.

Temperature changes appears alternately with altitude in the atmosphere from earth’s surface.

Correct option is A

The correct answer is (a).

Introduction 

A temperature inversion is an anomalous meteorological condition where the normal atmospheric lapse rate is reversed.

Instead of air cooling with increasing altitude, a layer of warmer air traps cooler air near the Earth's surface, acting like an impenetrable lid for vertical air movement.

Information Booster
  • Under normal tropospheric conditions, air temperature steadily decreases with altitude, allowing warm, polluted surface air to rise and disperse.
  • During an inversion, the cooler, denser air at the surface is trapped beneath a warmer aloft layer, completely halting atmospheric convection and vertical mixing.
  • Radiation inversions are common on clear, calm winter nights when the ground rapidly loses heat, cooling the air immediately above it.
  • Subsidence inversions occur in high-pressure systems when descending air masses compress and warm aloft.
  • Inversions are notorious for trapping primary pollutants and facilitating the photochemical reactions that create severe smog.
  • The Great Smog of London in 1952, which killed thousands, was directly caused by a prolonged, intense temperature inversion trapping domestic coal smoke.
Additional Knowledge
  • Option B describes an isothermal layer, a rare and usually thin atmospheric band where temperature remains constant with height, which is not an inversion.
  • Option C describes the standard, normal environmental lapse rate in the troposphere, where temperature decreases as altitude increases.
  • Option D describes an unstable, fluctuating atmospheric profile, not the distinct, stable boundary layer characteristic of a thermal inversion.

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