In the three-cell model, how is energy transfer from the equator toward higher latitudes explained?
Answer and explanation
Correct answer: By the combined effect of convection cells and mid-latitude waves
The global atmosphere redistributes surplus heat received in the tropics toward cooler higher latitudes. In the three-cell model, the Hadley and Polar cells transport energy through large-scale rising and sinking motions, while the Ferrel cell is strongly influenced by transient mid-latitude cyclones and waves rather than simple direct convection alone. These eddies and waves move sensible and latent heat poleward. Thus the combined role of circulation cells and mid-latitude waves makes option C the most complete answer.
Frequently asked questions
What is the correct answer to this question?
By the combined effect of convection cells and mid-latitude waves
Why is this the correct answer?
The global atmosphere redistributes surplus heat received in the tropics toward cooler higher latitudes. In the three-cell model, the Hadley and Polar cells transport energy through large-scale rising and sinking motions, while the Ferrel cell is strongly influenced by transient mid-latitude cyclones and waves rather than simple direct convection alone. These eddies and waves move sensible and latent heat poleward. Thus the combined role of circulation cells and mid-latitude waves makes option C the most complete answer.
Which subject and chapter does this question cover?
This is a Class 12 Geography question. Chapter: Atmospheric Circulation and Weather Systems.
Student feedback
Was this question useful?
👍 0 Helpful 👎 0 Not helpful
Yes 0% No 0%
0 responsesStudent Reviews
No published reviews yet.
