NDA Geography · Climatology, Atmosphere and Weather
Atmospheric Pressure and Winds
Differences in air pressure set air in motion, and the Earth's rotation (the Coriolis force) bends that motion — together they create the planetary wind belts, the geostrophic winds aloft, and the high-pressure anticyclones.
Why this matters
6 PYQs, several of them HARD, and the Coriolis force is the star: where it is strongest (the poles), why it is zero at the equator, and how it balances the pressure-gradient force to give geostrophic winds. Pair that with the pressure-belt picture and the anticyclone definition and you have the subtopic covered.
Concept 1 of 4: Pressure belts and planetary winds
Definition
The major pressure belts, equator to pole:
- Equatorial low (doldrums) — rising hot air, calm and rainy.
- Subtropical high (~30 deg, horse latitudes) — descending air, dry, source of trade winds and westerlies.
- Subpolar low (~60 deg) and polar high.
Planetary winds blow from high to low pressure, deflected by Coriolis:
- Trade winds — from subtropical highs toward the equatorial low.
- Westerlies — from subtropical highs toward the subpolar lows. The strong Southern-Hemisphere westerlies over open ocean are the Roaring Forties.
- Air pressure in India is measured in millibars (the usual unit).
Worked example
Practice this conceptself-check · 4 quick reps
The same idea in a real exam question:
Example 1 · Climatology, Atmosphere and Weather · Atmospheric Pressure and Winds
Westerlies blow WEST-to-EAST
Concept 2 of 4: The Coriolis force
Definition
- The Coriolis force deflects moving air: to the RIGHT in the Northern Hemisphere, to the LEFT in the Southern.
- It is largest at the poles and zero at the equator (it varies with the sine of the latitude).
- Because it is zero at the equator, wind there blows perpendicular to the isobars (straight across, undeflected) — NOTE the bank treats this 'wind perpendicular to isobars at the equator' as a SUBTLE/incorrect framing in one PYQ; what is unambiguously true is that Coriolis acts perpendicular to the pressure-gradient force.
- It arises purely from the Earth's rotation.
Worked example
Practice this conceptself-check · 3 quick reps
The same idea in a real exam question:
Example 2 · Climatology, Atmosphere and Weather · Atmospheric Pressure and Winds
Largest at the poles, zero at the equator
Concept 3 of 4: The geostrophic wind
Definition
- The geostrophic wind is the horizontal wind that results when the Coriolis force exactly balances the horizontal pressure-gradient force.
- It blows parallel to the isobars, above a height of about 600 m (above the friction layer).
- Statement II ('Coriolis balances the pressure force') is the correct EXPLANATION of statement I ('it blows parallel to the isobars above 600 m').
Worked example
Practice this concept3 quick reps
The same idea in a real exam question:
Example 3 · Climatology, Atmosphere and Weather · Atmospheric Pressure and Winds
Concept 4 of 4: Anticyclones
Definition
- An anticyclone is a HIGH-pressure system — correct.
- Air in its centre subsides (sinks) — correct.
- Its surface winds DIVERGE outward, NOT converge — so the claim 'characterised by converging winds' is FALSE (only cyclones have converging winds).
- Subsiding, warming air gives anticyclones their fair, settled weather.
Worked example
Practice this concept3 quick reps
The same idea in a real exam question:
Example 4 · Climatology, Atmosphere and Weather · Atmospheric Pressure and Winds
Anticyclone winds DIVERGE
Summary — formulas & gotchas at a glance
A revision cheat-sheet for the formulas and gotchas above. Click any concept name to jump back to its full explanation.
Watch out for (3)
- Westerlies blow WEST-to-EAST→ Pressure belts and planetary winds
- Largest at the poles, zero at the equator→ The Coriolis force
- Anticyclone winds DIVERGE→ Anticyclones
Test yourself on Climatology, Atmosphere and Weather
20 past NDA questions from this chapter, timed at 20 minutes and marked the way the exam marks it. You see your score and every answer the moment you finish. Free to start.