This lesson contains 25 slides, with interactive quizzes and text slides.
Lesson duration is: 30 min
Items in this lesson
PRECIPITATON
Slide 1 - Slide
What word does not belong in this row and why?
hail - cloud - snow - rain
Slide 2 - Open question
Slide 3 - Slide
Where is Cherrapunji ?
A
Asia
B
Europe
C
Africa
D
Northern America
Slide 4 - Quiz
Cherrapunji
Slide 5 - Slide
Types of precipitation
Goal:
Understand how the 3
types of precipitation
are formed.
Slide 6 - Slide
What are the steps that lead to precipitation? Show them in a drawing
Slide 7 - Open question
3 causes for rising air:
1. Air is pushed up by a mountain relief rainfall
2. Cold and warm air meet frontal rainfall
3. Warm/hot air is rising convectional rainfall
Slide 8 - Slide
1. Relief rainfall
windward side
wet air from sea
rain shadow
leeward side
dry air
Slide 9 - Slide
Slide 10 - Slide
2. Frontal rainfall
Warm air from the equator
meets cold air from the pole
Cold air is heavy and pushes
up the warm air.
Cools down-> rain
Slide 11 - Slide
Slide 12 - Slide
3. Convectional
rainfall
Warm air rises
Cools down Rain!
Around the equator, but also
hot summer days-> afternoon
Slide 13 - Slide
Slide 14 - Slide
Van links naar rechts
Slide 15 - Slide
Which type is the left one?
A
relief rainfall
B
convectional rainfall
C
condensation
D
frontal rainfall
Slide 16 - Quiz
Which type is the middle one?
A
relief rainfall
B
convectional rainfall
C
condensation
D
frontal rainfall
Slide 17 - Quiz
Which type is the right one?
A
relief rainfall
B
convectional rainfall
C
condensation
D
frontal rainfall
Slide 18 - Quiz
Which one do we have in the Netherlands most often? Also explain why.
Slide 19 - Open question
Frontale neerslag
Warme en koude lucht botsen tegen elkaar -> koude lucht is zwaar en de warme lucht is gedwongen op te stijgen. Als warme lucht opstijgt, koelt hij af. Hierdoor ontstaan er wolken en gaat het regenen.
Frontale regen komt veel veel in Nederland. Wij liggen aan zee en hebben geen bergen. Wel komt de wind bijna altijd uit het zuidwesten.
Een front = plek waar warme en koude lucht elkaar tegenkomen.
Slide 20 - Slide
Show a place where we have relief rainfall.
timer
1:00
Slide 21 - Open question
Andesgebergte -> stuwingsneerslag
Slide 22 - Slide
timer
1:00
Characteristics of areas with a lot of convectional rainfall.