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Chp 3: Weather and climate - Coggle Diagram

- - - - Altitude
        
        Higher altitude, lower temperature
      - Distance from sea
        
        Maritime effect vs Continental effect
      - Cloud cover
        
        Day and night, presence vs absence of clouds
      - Latitude
        
        Higher latitude, lower temperature
    - - 100% Relative humidity, amount of water vapor in air has reached the maximum that air can hold,
        fully saturated, leading to rain
    - - Earth's surface heated up. water evaporates and rise as water vapor, condense at dew point temperature to mass of water droplets in air
        Forming Cumulonimbus clouds
    - - Convectional rain
      - Relief rain
    - - Force exerted on earth's surface by weight of air above it, SI unit: Millibars
    - - Land and sea breeze due to uneven heating
      - Monsoon wind formed by Coriolis effect and Pressure difference
        
        Southwest monsoon, June to September
        
        Northeast monsoon, October to February
- - - - Kyoto protocol
    - - Singapore Green Plan(2012)
      - Green mark scheme
      - Plant-a-tree programme
- - - - Evacuation,medical aid