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Atmospheric Pressure Belts

Delhi Police & SSC Exams

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1. Introduction

The Earth's atmosphere is not uniform — it has different pressure zones formed due to uneven heating of the Earth's surface by the Sun.

These zones are known as Pressure Belts and they play a vital role in creating winds, rainfall, and global weather patterns.

Memory Tricks:

Low → High → Low → High → Low → High (From Equator to Poles)

Key Concepts:

  • Global pressure belt system
  • Air movement patterns
  • Wind formation and direction
  • Climate and weather influences

2. What Is Atmospheric Pressure?

Definition:

Atmospheric Pressure is the weight of the air exerted on the Earth's surface. It decreases with height and is highest at sea level.

Measured by: Barometer

Unit: Millibar (mb) or Hectopascal (hPa)

Key Facts:

Pressure decreases with altitude

Standard sea level pressure: 1013.25 mb

Low pressure = Rising air = Cloudy/rainy weather

High pressure = Sinking air = Clear/dry weather

3. Why Are Pressure Belts Formed?

Unequal Heating

Differential solar heating of Earth's surface

Earth's Rotation

Coriolis effect due to Earth's rotation

Convection Currents

Rising and sinking of air masses

Memory Trick: "HRC → Heating, Rotation, Convection"

4. Major Pressure Belts of the Earth

No. Pressure Belt Name Latitude Range Pressure Type Key Feature
1 Equatorial Low Pressure Belt 0°–5° N & S Low Rising warm air near equator
2 Subtropical High Pressure Belt 25°–35° N & S High Descending dry air
3 Subpolar Low Pressure Belt 55°–65° N & S Low Rising warm & cold air meeting
4 Polar High Pressure Belt Near 90° N & S High Very cold, dense air sinking

Memory Trick: "E–L, S–H, SP–L, P–H → 'Every Student Studies Patiently'"

5. Global Pressure Belts Diagram

Earth's Pressure Belts (Simplified)

90°N Polar High (H) Cold, dense air sinking
60°N Subpolar Low (L) Warm & cold air meeting
30°N Subtropical High (H) Descending dry air
Equatorial Low (L) Rising warm air
30°S Subtropical High (H) Descending dry air
60°S Subpolar Low (L) Warm & cold air meeting
90°S Polar High (H) Cold, dense air sinking

Important: Pressure belts are symmetrical on both sides of the Equator

6. Detailed Explanation of Each Belt

1. Equatorial Low-Pressure Belt (Doldrums)

Found between 0°–5° N & S. Air near the equator is heated, becomes light, and rises upward → creating a low-pressure zone.

Features: Area of calm winds and frequent rainfall

Memory Trick: "Equator = Rising air = Low pressure = Rain"

Also known as: Doldrums ("Calm Zone")

2. Subtropical High-Pressure Belt

Found around 30° N & S. Air that rose at the equator cools and sinks down here, creating high pressure.

Features: Regions are dry → Deserts (e.g., Sahara, Kalahari, Australian Desert)

Memory Trick: "30° = Sinking Air = Dry = Desert"

Also known as: Horse Latitudes

3. Subpolar Low-Pressure Belt

Found near 60° N & S. Warm westerlies meet cold polar winds → rising airlow pressure forms.

Features: Known for cyclonic activities and stormy weather

Memory Trick: "60° = Meeting Winds = Rising Air = Low Pressure"

4. Polar High-Pressure Belt

Found near 90° N & S (Poles). Air is extremely cold and dense, hence it sinks, forming high pressure.

Features: Winds blow outward from poles → Polar Easterlies

Memory Trick: "Poles = Cold = Heavy Air = High Pressure"

7. Relation Between Pressure Belts and Winds

Basic Principle:

Winds always blow from High Pressure → Low Pressure

Global Wind Systems:

Trade Winds (from Subtropical High → Equatorial Low)

Westerlies (from Subtropical High → Subpolar Low)

Polar Easterlies (from Polar High → Subpolar Low)

Wind Flow Pattern:

High Pressure Zones

Low Pressure Zones

Wind Direction

Memory Trick: "H → L = Wind Flow Rule"

8. Shifting of Pressure Belts

Seasonal Movement:

  • Pressure belts shift northward in summer
  • Pressure belts shift southward in winter
  • Due to apparent movement of the Sun

Impact: This shifting causes seasonal changes and influences monsoon winds in India

Movement Pattern:

June: Sun overhead at Tropic of Cancer → Belts shift north

December: Sun overhead at Tropic of Capricorn → Belts shift south

March/September: Sun at Equator → Belts in normal position

Memory Trick: "Sun moves → Belts move → Seasons change"

9. Importance of Pressure Belts

Control global wind systems

Influence ocean currents

Affect rainfall & weather

Responsible for monsoon circulation

Define desert and rainy zones

Influence human settlement patterns

PYQs (Delhi Police, SSC & State Exams)

1

The equatorial low-pressure belt is also known as —

Options: (a) Trade Wind Belt (b) Westerly Belt (c) Doldrums (d) Horse Latitude

Category: Pressure Belt Names

Show Answer

c) Doldrums

2

Which pressure belt is associated with desert regions?

Options: (a) Subpolar Low (b) Subtropical High (c) Equatorial Low (d) Polar High

Category: Pressure Belt Features

Show Answer

b) Subtropical High

3

The area around 30° latitude is known for —

Options: (a) Calm and rainy weather (b) High temperature and humidity (c) Dry and descending air (d) Low-pressure cyclones

Category: Pressure Belt Characteristics

Show Answer

c) Dry and descending air

4

The polar high-pressure belt is characterized by —

Options: (a) Warm and moist air (b) Cold and dense air (c) Hot and dry air (d) Rising air currents

Category: Polar Belt Features

Show Answer

b) Cold and dense air

5

Winds blow from —

Options: (a) Low pressure to high pressure (b) High pressure to low pressure (c) Equator to poles only (d) Poles to equator only

Category: Wind Direction Principle

Show Answer

b) High pressure to low pressure

6

The meeting zone of westerlies and polar easterlies is —

Options: (a) Equatorial Low Belt (b) Subtropical High Belt (c) Subpolar Low Belt (d) Polar High Belt

Category: Wind Systems

Show Answer

c) Subpolar Low Belt

7

Horse Latitudes are associated with —

Options: (a) Subpolar Low Pressure (b) Subtropical High Pressure (c) Polar High Pressure (d) Equatorial Low Pressure

Category: Alternative Names

Show Answer

b) Subtropical High Pressure

10. Quick Summary Table

Pressure Belt Latitude Pressure Air Movement Other Name / Feature
Equatorial Low (Doldrums) 0°–5° Low Rising air Heavy rainfall, calm
Subtropical High (Horse Lat.) 25°–35° High Descending air Deserts, dry winds
Subpolar Low 55°–65° Low Rising air Cyclonic storms
Polar High 90° High Descending air Cold, dry winds

Final Exam Tips

Remember: Low–High–Low–High–Low–High pattern

Doldrums → Equatorial Low

Horse Latitudes → Subtropical High

Deserts → Found near 30° latitude

Polar = High pressure = Cold air

Winds blow from High → Low pressure

Memory Trick: "LHLHLH – Daring Students Learn Helpful Habits"

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