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.
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