Les 7.5 - §3.4 Precipitation

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Slide 1: Link
AardrijkskundeMiddelbare schoolvwoLeerjaar 2

This lesson contains 14 slides, with interactive quizzes and text slides.

time-iconLesson duration is: 45 min

Items in this lesson

Slide 1 - Link

Planning
  • Three different ways precipitation forms
  • We are going to use windy to find the ways precipitation forms

Slide 2 - Slide

Learning goals
  • Je weet dat waterstress door fysieke en economische watertekorten kan ontstaan.
  • Je begrijpt waarom toenemende waterstress tot een wateroorlog kan leiden.
  • Je kunt een aantal maatregelen noemen om om te gaan met watertekort
  • Je begrijpt de drie treden van de drietrapsstrategie, en hoe ze overstromingen voorkomen

Slide 3 - Slide

Three types of rain
  • Convectional rain (stijgingsregen)
  • Frontal rain (Frontale regen)
  • Relief rain (stuwingsregen)

Slide 4 - Slide

Slide 5 - Slide

Convectional rain (stijgingsregen)
Hot air rises. The higher, the colder. The water vapour in the rising air starts to condense. Which leads to rain we call convectional rainfall.

Slide 6 - Slide

Slide 7 - Link

Give an example of convectional rain using a screenshot of Windy.com

Slide 8 - Open question

Where does rain occur?

Slide 9 - Mind map

Frontal rain (Frontale regen)
At temperate latitudes (gematigde breedte), warm air from low latitudes clash against cold air from polar regions, the warm air is forced to rise and frontal rain forms.

Slide 10 - Slide

Give an example of frontal rain using a screenshot of Windy.com

Slide 11 - Open question

Relief rain (stuwingsregen)
When air is blown against mountains, the air is forced to rise, cools down and condenses. Leading to rainfall. This rain is called relief rainfall. On the other side of the mountains, it is dry, because the clouds have already emptied themselves of rain.

Slide 12 - Slide

Give an example of relief rain using a screenshot of Windy.com

Slide 13 - Open question

Slide 14 - Slide