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Cloud patterns & impact on India’s Monsoon dynamics

Context

A recent study shows that during India’s summer monsoon, deep convective clouds (which bring heavy rain) have risen by about 1 km in the last 20 years. This means more intense monsoon rains and extreme weather events like floods and heavy storms.

Why is this Happening?

  • Warmer Oceans: The Indian Ocean’s rising temperature is fueling stronger cloud formation.
  • Increased Convection: More heat and moisture lead to taller clouds, which bring more intense rainfall.

Impact on India

  • More Floods in Northwest India: Stronger monsoon storms increase flooding risks in states like Rajasthan, Punjab, and Himachal Pradesh.
  • Heavier Rain on Coastal Regions:
    • Western Coast (Kerala, Karnataka, Maharashtra) sees intense rainfall due to warm ocean air.
    • Eastern Coast (Odisha, Andhra Pradesh, West Bengal) experiences stronger storms.
  • Increased Rain in Northeast India: States like Assam, Meghalaya, and Arunachal Pradesh may see more intense rainfall.

Fact Box:

Types of Clouds (Based on Height and Appearance)

A. High Clouds (Above 6,000 meters)

  • Cirrus – Wispy, feather-like clouds; indicate fair weather but may signal storms.
  • Cirrostratus – Thin, sheet-like clouds covering the sky; cause a "halo" around the sun/moon.
  • Cirrocumulus – Small, white patches in a wave pattern; called "mackerel sky".

B. Middle Clouds (2,000–6,000 meters)

  • Altostratus – Grayish cloud layers covering the sky; bring light rain.
  • Altocumulus – White or gray patches in groups; indicate weather change.

C. Low Clouds (Below 2,000 meters)

  • Stratus – Uniform, gray clouds covering the sky; cause light drizzle.
  • Stratocumulus – Low, lumpy clouds; can bring light rain but mostly dry.
  • Nimbostratus – Thick, dark clouds bringing continuous rain or snow.

D. Vertical Clouds (Can Grow from Low to High Levels)

  • Cumulus – Puffy, white clouds with a flat base; indicate fair weather.
  • Cumulonimbus (Deep Convective Clouds) – Towering clouds with an anvil-shaped top; bring thunderstorms, heavy rain, hail, or tornadoes.

Deep Convective Clouds

  • These are large towering clouds that reach high into the atmosphere.
  • They form due to strong rising air (convection) caused by heat and moisture. They bring heavy rain, thunderstorms, and extreme weather events.

Indian Monsoon

  • The monsoon is a seasonal wind pattern that brings heavy rains to India, especially in summer. It has two phases:
  • Southwest Monsoon (June–September): Brings rainfall to most of India (majority of annual rainfall). It is the main rainy season.
  • Northeast Monsoon (October–December): Brings rainfall mainly to Tamil Nadu and South India.
  • Formation Mechanism:
    • Heat and Low Pressure: During summer, the Indian landmass heats up more than the surrounding oceans. This creates a low-pressure area over northern India and Central Asia.
    • Moist Air Influx: Moist air from the Indian Ocean is drawn towards this low-pressure area. As the moist air reaches land, it is forced to rise.
    • Cloud Formation and Rain: As the air rises, it cools down, forming clouds. The cooling causes water vapor to condense into rain, leading to heavy downpours.
  • Wind Reversal:
    • Before Monsoon, winds blow from the northeast.
    • During Monsoon, the wind direction reverses (to the southwest), bringing in moist air from the ocean.
    • After Monsoon, when the land cools down with the onset of winter, winds reverse again (to the northeast), marking the retreat of the monsoon.
  • Climate pattern impacting Monsoon: El Nino, La Nina, Indian Ocean Dipole, Oscillations; and Jet Stream, etc.
PYQ

Q. How far do you agree that the behavior of the Indian monsoon has been changing due to humanizing landscape? Discuss. (2015)

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