Clouds
Clouds
Formation
Basic Process
Evaporation (Water Vapor Rises)
Cooling of Air
Condensation into Droplets
Cloud Formation
Key Conditions
Moisture in Air
Cooling Mechanism
Condensation Nuclei (Dust, Particles)
Lifting Mechanisms
Convection (Warm Air Rising)
Orographic Lift (Mountains)
Frontal Lift (Air Mass Interaction)
Convergence (Airflows Meet)
Types of Clouds
High-Level Clouds (>6000m)
Cirrus (Thin, Wispy, Ice Crystals)
Cirrostratus (Thin Layer, Halo Effects)
Cirrocumulus (Small Ripples, Grainy)
Mid-Level Clouds (2000–6000m)
Altostratus (Gray, Uniform Layer)
Altocumulus (Patchy, Rounded Clouds)
Low-Level Clouds (<2000m)
Stratus (Flat, Overcast Layer)
Stratocumulus (Low, Lumpy Clouds)
Nimbostratus (Thick, Rain Clouds)
Vertical Development
Cumulus (Fluffy, Fair Weather)
Cumulonimbus (Thunderstorms, Heavy Rain)
Characteristics
Composition
Water Droplets
Ice Crystals
Mixed Phase
Appearance
Shape (Layered, Puffy, Wispy)
Color (White, Gray, Dark)
Density & Thickness
Weather Indicators
Cirrus → Fair Weather or Change Coming
Cumulus → Stable Conditions
Cumulonimbus → Storms
Nimbostratus → Continuous Rain
Environmental Role
Climate Impact
Reflect Sunlight (Cooling Effect)
Trap Heat (Greenhouse Effect)
Water Cycle
Precipitation Source
Transport of Moisture