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CDS Geography · Climatology, Atmosphere and Weather

Pressure, Winds and Cyclones

What makes wind blow and turn, the pressure belts and the three cells that set the planetary winds, the names cyclones go by, and the local winds CDS asks about.

Why this matters

Eleven CDS questions from 2018 to 2025: 2 EASY, 9 MODERATE. Six are about pressure and the planetary winds, two about cyclones and three about local winds and storms. The Coriolis force and the Hadley cell are the two ideas the statement items keep testing.

Concept 1 of 4: Pressure gradient and the Coriolis force

Air moves from high pressure to low pressure, and the bigger the difference over a short distance, the stronger the wind. But the Earth spins under the moving air, so the wind does not go straight: it is turned to one side. That turning is the Coriolis force.

Definition

Forces that shape the wind:

  • Isobars are lines joining places of equal pressure. Closely spaced isobars show a steep pressure gradient and strong winds; widely spaced isobars show a gentle gradient and light winds.
  • The Coriolis force comes from the Earth's rotation. It turns the wind to the right in the northern hemisphere and to the left in the southern hemisphere.
  • It is zero at the equator and greatest at the poles (it grows with latitude).
  • Cold land builds high pressure. In winter a high forms over north-west India, so a place like Jaisalmer has higher winter pressure than Chennai or Guwahati. High places like Leh have low pressure because there is less air above them.
FeatureFact
Strong pressure gradient on a weather mapClosely spaced isobarsQ
CDS 2024 (II): closely spaced isobars, not widely spaced ones.
Coriolis deflection, northern hemisphereTo the right
Coriolis deflection, southern hemisphereTo the left
Coriolis force at the equatorZero
Coriolis force at the polesGreatest
Highest winter pressure in IndiaThe north-west, for example JaisalmerQ
CDS 2018 (I): Jaisalmer, ahead of Leh, Chennai and Guwahati.
Practice this conceptself-check · 4 quick reps

The same idea in a real exam question:

CDS · 2021 · CDS (I) 2021 — General Knowledge · Q43Moderate

Example 1 · Climatology, Atmosphere and Weather · Pressure, Winds and Cyclones

Which one of the following statements about the Coriolis force is not correct ?

Left in the south, right in the north

The Coriolis force turns winds to the right in the northern hemisphere and to the left in the southern. A statement that it turns winds to the right in the southern hemisphere is false.

No Coriolis force at the equator

The Coriolis force is zero at the equator and greatest at the poles. This is why tropical cyclones never form right on the equator.

Concept 2 of 4: Pressure belts and the three cells

The equator is heated most, so air there rises. It flows towards the poles high up, cools, and sinks around 30° latitude, then flows back to the equator along the ground. That loop is the Hadley cell, and the surface part of it is the trade winds. Two more loops, the Ferrel and polar cells, complete the pattern up to the poles.

Definition

The global pattern:

  • Equatorial low (0 to 5°): hot air rises; calm air called the doldrums; the trade winds meet here at the ITCZ (Inter-Tropical Convergence Zone).
  • Subtropical highs (about 30°): air that rose at the equator sinks here. Most hot deserts lie under them.
  • Subpolar lows (about 60°) and polar highs.
  • Trade winds blow from the subtropical highs to the equator; westerlies from the subtropical highs towards the subpolar lows; polar easterlies from the poles.
  • Hadley cell (0 to 30°): driven by heating at the equator. Ferrel cell (30 to 60°). Polar cell (60 to 90°).
  • NCERT: the pattern of planetary winds depends on latitudinal variation of heating, the pressure belts and their seasonal shift with the Sun, the distribution of continents and oceans, and the rotation of the Earth.
Belt or cellLatitudeWhat happens
Equatorial low (doldrums, ITCZ)0 to 5°Hot air rises; trade winds meet
Subtropical highAbout 30°Air of the Hadley cell sinksQ
CDS 2020 (I): Hadley cell air rises at the equator and descends at the subtropical high-pressure cells.
Subpolar lowAbout 60°Westerlies and polar easterlies meet
Polar highAbout 90°Cold air sinks
Hadley cell0 to 30°Driven by strong heating at the equator; gives the trade winds
Ferrel cell30 to 60°Gives the westerlies
Polar cell60 to 90°Gives the polar easterlies
Practice this conceptself-check · 4 quick reps

The same idea in a real exam question:

CDS · 2020 · CDS (I) 2020 — General Knowledge · Q68Moderate

Example 2 · Climatology, Atmosphere and Weather · Pressure, Winds and Cyclones

In the Hadley cell thermal circulation, air rises up and finally descends at

Hadley air sinks at 30°, not at the equator

The ITCZ, doldrums and equatorial trough are where Hadley cell air rises. It descends at the subtropical high-pressure belts near 30°.

All the listed factors count

NCERT names heating by latitude, the distribution of continents and oceans, and the rotation of the Earth among the factors behind the planetary winds. A statement item listing all three expects all three.

Concept 3 of 4: Tropical and temperate cyclones

A cyclone is a low-pressure centre with winds spiralling into it. Tropical cyclones are born over warm seas and are steered westward by the trade winds. Temperate cyclones form where warm and cold air masses meet, and the westerlies carry them eastward. The same storm has different names in different oceans.

Definition

What every cyclone shares, and how the two kinds differ:

  • Every cyclone has low pressure at the centre, ringed by closed isobars. (High pressure at the centre is an anticyclone.)
  • Winds turn anticlockwise round a cyclone in the northern hemisphere and clockwise in the southern.
  • Tropical cyclones form over warm seas (above about 27 °C), move east to west with the trade winds, and have a calm, clear centre called the eye.
  • Temperate cyclones form along fronts in the middle latitudes and move west to east with the westerlies.
NameWhere
CyclonesIndian Ocean
HurricanesAtlantic Ocean and the Caribbean
TyphoonsWestern Pacific and South China Sea
Willy-williesOff north-western Australia
Practice this conceptself-check · 4 quick reps

The same idea in a real exam question:

CDS · 2021 · CDS (I) 2021 — General Knowledge · Q71Moderate

Example 3 · Climatology, Atmosphere and Weather · Pressure, Winds and Cyclones

Match List I with List II and select the correct answer using the code given below the lists :
List IList II
A. Cyclones1. Western Australia
B. Hurricanes2. South China Sea
C. Typhoons3. Indian Ocean
D. Willy-willies4. Atlantic Ocean
Code :

The eye is the centre, not the front

The eye of a cyclone is its calm centre, where the air sinks and the sky clears. It is not the front edge of the storm.

Hurricanes are tropical

Hurricanes are tropical cyclones of the Atlantic. They form over warm tropical seas, not in the middle latitudes.

Concept 4 of 4: Local winds and storms

Local winds are set up by the land around them: a cold mountain draining air into a warm coast, a hot plain baking under the summer Sun, a sea breeze meeting a hot land. CDS asks you to put each name in its place.

Definition

Named winds and storms:

  • Bora: a cold, dry wind blowing down from the mountains onto the eastern shore of the Adriatic Sea.
  • Mistral: a cold wind blowing down the Rhone valley in France.
  • Bise: a cold, dry wind of Switzerland.
  • Loo: a hot, dry wind over the plains of north India in summer afternoons.
  • Kalbaisakhi (Nor'westers): violent evening thunderstorms of West Bengal and Assam before the monsoon.
  • Mango showers: NCERT's name for the pre-monsoon showers common in Kerala and coastal Karnataka at the end of summer, which help mangoes ripen early. NCERT also names blossom showers, which make coffee flowers blossom in Kerala and nearby areas.
  • Blizzard: a violent snowstorm with strong wind, found in high snowy mountains and polar lands. In India, the Himalayan heights of states such as Arunachal Pradesh.
Wind or stormKindWhere
BoraCold, dry, blows down the mountainsEastern shore of the Adriatic SeaQ
CDS 2020 (I): Bora, not the Mistral or the Bise.
MistralColdRhone valley, France
BiseCold, drySwitzerland
LooHot, dry, summer afternoonsPlains of north India
KalbaisakhiEvening thunderstorms before the monsoonWest Bengal and Assam
Mango showersPre-monsoon showersKerala and coastal Karnataka
BlizzardViolent snowstormHigh snowy mountains and polar landsQ
CDS 2021 (II): of four states, only Arunachal Pradesh, with its high Himalaya, needs a blizzard warning.
Practice this conceptself-check · 4 quick reps

The same idea in a real exam question:

CDS · 2020 · CDS (I) 2020 — General Knowledge · Q37Moderate

Example 4 · Climatology, Atmosphere and Weather · Pressure, Winds and Cyclones

In the region of eastern shore of Adriatic Sea, a cold and dry wind blowing down from the mountain is known as

Bora and Mistral are different valleys

Both are cold winds draining off mountains. The Bora reaches the Adriatic coast; the Mistral blows down the Rhone valley of France.

Kalbaisakhi is Bengal, mango showers are the south-west

Kalbaisakhi storms belong to West Bengal and Assam. The pre-monsoon showers of Kerala and coastal Karnataka are the mango showers.

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.

Reference tables (4)

Pressure gradient and the Coriolis force6 rows
FeatureFact
Strong pressure gradient on a weather mapClosely spaced isobarsQ
CDS 2024 (II): closely spaced isobars, not widely spaced ones.
Coriolis deflection, northern hemisphereTo the right
Coriolis deflection, southern hemisphereTo the left
Coriolis force at the equatorZero
Coriolis force at the polesGreatest
Highest winter pressure in IndiaThe north-west, for example JaisalmerQ
CDS 2018 (I): Jaisalmer, ahead of Leh, Chennai and Guwahati.
Pressure belts and the three cells7 rows
Belt or cellLatitudeWhat happens
Equatorial low (doldrums, ITCZ)0 to 5°Hot air rises; trade winds meet
Subtropical highAbout 30°Air of the Hadley cell sinksQ
CDS 2020 (I): Hadley cell air rises at the equator and descends at the subtropical high-pressure cells.
Subpolar lowAbout 60°Westerlies and polar easterlies meet
Polar highAbout 90°Cold air sinks
Hadley cell0 to 30°Driven by strong heating at the equator; gives the trade winds
Ferrel cell30 to 60°Gives the westerlies
Polar cell60 to 90°Gives the polar easterlies
Tropical and temperate cyclones4 rows
NameWhere
CyclonesIndian Ocean
HurricanesAtlantic Ocean and the Caribbean
TyphoonsWestern Pacific and South China Sea
Willy-williesOff north-western Australia
Local winds and storms7 rows
Wind or stormKindWhere
BoraCold, dry, blows down the mountainsEastern shore of the Adriatic SeaQ
CDS 2020 (I): Bora, not the Mistral or the Bise.
MistralColdRhone valley, France
BiseCold, drySwitzerland
LooHot, dry, summer afternoonsPlains of north India
KalbaisakhiEvening thunderstorms before the monsoonWest Bengal and Assam
Mango showersPre-monsoon showersKerala and coastal Karnataka
BlizzardViolent snowstormHigh snowy mountains and polar landsQ
CDS 2021 (II): of four states, only Arunachal Pradesh, with its high Himalaya, needs a blizzard warning.

Watch out for (8)

Test yourself on Climatology, Atmosphere and Weather

15 past CDS questions from this chapter, timed at 15 minutes and marked the way the exam marks it. You see your score and every answer the moment you finish. Free to start.