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Geography Class 9 Maharashtra Board | Menu
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Geography Notes Chapter 5 Precipitation Class 9 Maharashtra Board

Introduction


What is Precipitation?

  • Precipitation is when water falls from clouds to the ground in solid or liquid forms.
  • Examples: Snow, hailstones, rainfall.
  • It happens because of water vapor in the air changing due to temperature and pressure.

Water on Earth

  • 70.8% of Earth’s surface is covered with water.
  • Water is not spread evenly-some places have a lot, some have very little.
  • Water vapor in the air turns into different forms like dew, fog, snow, or rain depending on the weather.

Forms of Precipitation


Snow


How it Forms:

  • When the air temperature drops below 0°C (freezing point), water vapor turns directly into snowflakes (called sublimation).
  • This happens without becoming liquid first-gas turns straight to solid.

Where it Happens:

  • Common in high-latitude areas (like Kashmir) and high-altitude places above the snowline.
  • Tropical areas like Maharashtra don’t get snow at sea level because it’s too warm.

Features:

  • Snow is soft, flaky, and opaque (not see-through).
  • It piles up in layers and doesn’t flow like water.

Effects:

  • Heavy snow can block roads and communication.
  • People need protection from frostbite (cold injury).
  • Melting snow provides water to the region.

Snow vs. Ice:

  • Snow turns into ice when lower layers get pressed by upper layers, becoming hard and transparent.

Hail


How it Forms:

  • Hot air rises fast from the Earth’s surface, carrying water vapor upward.
  • The air cools at higher altitudes, forming dark clouds.
  • Water droplets freeze into hailstones due to cold temperatures and strong winds.
  • Hailstones grow bigger as more layers of ice form around them.

Where it Happens:

  • Seen in summers in India, Africa, and Southeast Asia.
  • Doesn’t happen in equatorial areas (too hot) or cold zones (no strong upward air).

Features:

  • Hailstones are heavy and solid, falling fast to the ground.
  • They have concentric layers (like onion rings) from repeated freezing.

Effects:

  • Can destroy crops and damage property or even hurt people.

Rainfall


How it Forms:

  • Warm air with water vapor rises, cools, and condenses into tiny water droplets.
  • These droplets join dust particles to form clouds.
  • When droplets get too heavy, they fall as rain.

Types of Rainfall:


Convectional Rainfall:

  • Happens in hot equatorial areas (e.g., Congo Basin, Amazon Basin).
  • Sun heats the ground, warm air rises, cools, and causes rain, often with thunder and lightning.
  • Common in afternoons daily in these regions.

Orographic Rainfall:

  • Moisture-laden winds from seas or lakes hit mountains and rise.
  • Air cools as it rises, condenses, and rains on the windward side (facing the wind).
  • The leeward side (opposite) gets less rain, called the rain shadow area.
  • Example: Western Ghats in Maharashtra get more rain on the west side.

Cyclonic Rainfall:

  • Occurs in low-pressure areas called cyclones.
  • Air moves to the center, rises, cools, and rains.
  • Common in temperate zones, often with stormy winds and floods.

Other Forms of Condensation (Near the Surface)


Fog

How it Forms:

  • Air near the ground cools, and water vapor turns into tiny floating droplets.
  • When these droplets get dense, fog forms, reducing visibility.

Where it Happens:

  • Seen in winter, e.g., London has thick fog till afternoon.
  • Less dense in tropical areas like India due to warmer weather.

Dew

How it Forms:

  • Moist air touches cold objects (like grass) at night, turning vapor into small water droplets.

Where it Happens:

  • Common on winter mornings in many places.

Frost

How it Forms:

  • When temperature drops below 0°C, dew droplets freeze into frost.

Where it Happens:

  • Seen in cold winter areas on surfaces like grass or roads.

How to Measure Precipitation


Rain Gauge

What it is:

  • A tool to measure rainfall, with a funnel and a bottle to collect water.

How it Works:

  • Rain falls into the funnel and collects in the bottle.
  • Water is measured in millimeters (mm) using a measuring jar.
  • In heavy rain areas, readings are taken every 3 hours.

Precautions:

  • Place it in an open area, 30 cm above ground, to avoid obstructions.

Fun Fact:

  • 1 mm rain over 1 sq.km = 10 lakh liters of water!

Measuring Snowfall

Melt the snow in the rain gauge container and measure the water.

120 mm of snow equals 10 mm of rainfall.


Special Rainfall: Acid Rain


What it is:

  • Rainfall mixed with acids (like nitric or sulfuric acid) due to air pollution.

How it Forms:

  • Polluted gases from industries mix with water vapor, forming acidic rain.

Effects:

  • Harms plants, animals, buildings, and human health.

Effects of Precipitation


Positive Effects:

  • Main source of drinking water.
  • Good rainfall at the right time boosts crop growth (important for India’s farmers).
  • Melting snow provides water in some regions.

Negative Effects:

  • Too Much Rain:
    • Floods destroy homes, crops, and lives.
  • Too Little Rain:
    • Droughts cause food shortages and economic problems.
  • Fog:
    • Reduces visibility, causing transport delays or accidents.
  • Frost:
    • Damages crops and makes roads slippery.
  • Hail:
    • Breaks crops and property.

India’s Rainfall:

  • Monsoons are key for agriculture, but rain is uneven and unpredictable.
  • Good rain helps; untimely rain harms crops.

Why Rainfall Varies


Factors Affecting Rainfall:

  • Amount of water vapor in the air.
  • Air pressure (low pressure = more rain).
  • Temperature (cooler air holds less moisture).
  • Topography (mountains cause orographic rain).
  • Latitude (tropical areas get more rain).

Examples:

  • High rain in tropical areas due to heat and moisture.
  • Less rain in eastern Europe due to distance from oceans.
  • Eastern Australia gets more rain due to coastal winds.

Activities and Experiments


Make Rain Experiment:

  • Materials: Glass container with metal lid, nail, hammer, hot water, ice cubes, salt.
  • Steps:
    • Punch small dents in the lid (no holes).
    • Fill 1/3 of the container with steamed water.
    • Close lid tightly, add ice cubes, salt, and a little water on top.
    • Wait 10-15 minutes to see “rain” droplets fall inside.
  • Explanation:
    • Steam rises, cools on the cold lid, forms droplets, and falls like rain.

Measure Rainfall:

  • Use a rain gauge at school for one week.
  • Record daily rain in mm and make a bar graph.

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