Lesson 21,22,23

Cards (22)

  • Weather - conditions of the atmosphere over a short period of time
  • Climate - how the atmosphere behaves over a long period of time and space
  • Forecast - scientific prediction of the weather conditions in the future
  • Thunderstorms - weather disturbances that brings heavy rain, sometimes accompanied by thunder and lightning
  • Red
    • More than 30 mm of rain
    • serious flooding
    • evacuate immediately
  • Orange
    • 15-30 mm intense rain
    • Flooding is threatening
    • Alert for possible evacuation
  • Yellow
    • 7-15 mm heavy rain
    • Flooding is possible
    • Monitor weather condition
  • What are the two types of breeze?
    Land breeze, sea breeze
  • What type of breeze usually happens during the day?
    Sea breeze
  • The sea breeze blows from sea to land, cooling the land and bringing moisture from the sea.
  • What type of breeze occurs during the night?
    Land breeze
  • Land breeze flows from the land to the sea, bringing warm air from the land and cool air from the sea.
  • Warm air can rise over the land during the day and cool air can sink over the land at night.
  • What is a convection cell?

    A circular pattern of air or water movement caused by temperature differences.
  • Land =
    Day: high temperature, low pressure
    Night: low temperature, high pressure
  • Sea=
    Day: low temperature, high pressure
    Night: high temperature,low pressure
  • What are monsoons?

    Seasonal winds that bring heavy rainfall, especially in South and Southeast Asia.
  • What does ITCZ stand for?
    Intertropical Convergence Zone
  • Amihan:
    • November-February
    • Cold and relatively dry air
    • Central and western part of Luzon and Visayas
  • Habagat:
    • June-September
    • Heavy rains, warm and moist air
    • Western sections of Southern Luzon, Visayas, and Mindanao
  • How does Amihan work?
    Air mass moves and gathers moisture before reaching and affecting the eastern parts of the country
  • How does Habagat work?
    Relatively warmer air in the continent rises and creates a low-pressure area which enables the moisture bearing winds.