This lesson contains 14 slides, with interactive quizzes and text slides.
Lesson duration is: 45 min
Items in this lesson
jeugdjournaal.nl
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
www.windy.com
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