Formation Process: Clouds form when water vapor in the air condenses to create liquid water or ice crystals.
Condensation: Molecules of water vapor transition to liquid water during this process.
Requirements for Condensation: Two key conditions are essential for condensation to take place:
Cooling of Air: Warm, moist air rises from the Earth's surface and cools as it ascends.
Presence of Particles: Tiny particles in the air facilitate the condensation of water vapor.
Steps of Cloud Formation:
Warm, moist air rises and cools.
Upon reaching a certain height, the air cools to the dew point.
Water vapor condenses onto airborne particles, forming a cloud.
Cirrus Clouds:
Meaning: "Curls of hair."
Characteristics: Wispy, feathery and high-altitude clouds composed of ice crystals.
Cumulus Clouds:
Meaning: "Heap" or "mass."
Characteristics: Fluffy, rounded clouds resembling cotton, typically growing in size.
Stratus Clouds:
Meaning: "Spread out."
Characteristics: Form in flat layers, usually covering the sky in a uniform dull gray.
Cloud Classifications: Clouds can be categorized further based on altitude:
Alto- Clouds (meaning: "high"; mid-level clouds)
Nimbus- Clouds (meaning: "rain"; associated with precipitation)
Layered Structure: Clouds can be arranged in layers.
Exceptions to Nature of Clouds:
Puffy: Cumulonimbus
High: Cirrostratus, Cirrus, Cirrocumulus
Middle: Altostratus, Nimbostratus, Altocumulus
Low: Stratus, Stratocumulus, Cumulus
High Clouds:
Cirrostratus
Cirrus
Cirrocumulus
Middle Clouds:
Nimbostratus
Low Clouds:
Altostratus
Altocumulus
Stratocumulus
Cumulus
Cumulonimbus
Stratus
Cloud Visuals: High clouds may appear in separate patches or waves.
Visibility: Sunlight can be visible through certain cloud layers, but they may appear blurred or fuzzy.
High Clouds:
Cirrostratus
Cirrus
Cirrocumulus
Middle Clouds:
Nimbostratus
Low Clouds:
Altostratus
Altocumulus
Stratocumulus
Cumulus
Cumulonimbus
Stratus