2.4 Precipitation

PRECIPITATON
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Slide 1: Slide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 1

This lesson contains 25 slides, with interactive quizzes and text slides.

time-iconLesson 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.

Slide 23 - Mind map

Tropisch regenwoud

Slide 24 - Slide

Goal: understand formation of 3 types of rainfall



               THE END



Slide 25 - Slide