§3.4: water: too much or too little - part 2

§3.4: water: too much or too little
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Slide 1: Diapositive
AardrijkskundeMiddelbare schoolvwoLeerjaar 2

Cette leçon contient 21 diapositives, avec quiz interactifs, diapositives de texte et 1 vidéo.

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§3.4: water: too much or too little

Slide 1 - Diapositive

Today
  • Recap previous lesson
  • Explanation §3.4
  • Assignments workbook

Slide 2 - Diapositive

Water

Slide 3 - Diapositive

Explain in 5 steps how clouds are formed
timer
1:00

Slide 4 - Question ouverte

The formation of clouds

Slide 5 - Diapositive

The sun heats the ocean, the water from the ocean .. 1 .. . The air with .. 2 .. rises. As the air rises, it .. 3 .. . High up in the air, water vapour .. 4 .. to form clouds. If the drops of water become too heavy, it starts raining or snowing: this is .. 5 ... 
timer
1:30
precipitation
condenses
evaporates
cools down
water vapor
1
2
3
4
5

Slide 6 - Question de remorquage

Where do you see:
  • Short water cycle
  • Long water cycle

Explain the difference 
between:
  • Evaporation
  • Condensation
  • Precipitation
  • Infiltration

Slide 7 - Diapositive

Today
  • Recap previous lesson
  • Explanation §3.4
  • Assignments workbook

Slide 8 - Diapositive

Learning goals
  • You understand how relief rainfall, convectional rainfall and frontal rainfall are being formed
  • You can point out the regions with high and low precipitation on a map 

Slide 9 - Diapositive

Vocabulary 
Precipitation
Neerslag
Convectional rainfall
Stijgingsregen
Relief rainfall
Stuwingsregen
Frontal rain
Frontale regen
Humid 

Vochtig
Windward side
Loefzijde 
Leeward side 
Lijzijde
Descending air
Dalende lucht

Slide 10 - Diapositive

Precipitation
  • Convectional rainfall: rain that  forms when it is very hot and a lot of water evaporates and rises
  • Relief rainfall: rain that forms when air is blown against a mountain and is forced to rise 
  • Frontal rainfall: rain formed because warm and cold air meet.


Precipitation always needs rising air!

Slide 11 - Diapositive

1: Convectional rainfall (stijgingsregen)

  1. Hot air rises 
  2. The higher the colder
  3. The water vapor in the rising air condenses 
  4. Clouds are formed
  5. Water droplets accumulate > precipitation 

Slide 12 - Diapositive

2: Relief rainfall (sturingsregen)

  1. Air is blow against a mountain
  2. The air is forced to rise
  3. The air cools down and condenses > precipitation

Other side of the mountain: dry, descending air 

Slide 13 - Diapositive

Slide 14 - Diapositive

3: Frontal rain 
(frontale regen)
  1.  Warm air from low latitudes collides with cold air from polar regions
  2. The warm air is forced to rise > precipitation 

Slide 15 - Diapositive

0

Slide 16 - Vidéo

Match the concepts and the definitions by dragging the concept to the right definition
timer
1:00
Rain that forms when it is very hot and a lot of water evaporates and rises.
The process in which sea water evaporates and falls back into the sea through clouds and precipitation.
The process in which seawater evaporates and flows back to the sea through clouds, precipitation, groundwater and rivers.
Rain that forms when air is blown against a mountain and is forced to rise.
Rain that forms when two air masses meet and one air mass rises over the other
Relief rainfall
Convectional rainfall
Long water cycle
Short water cycle
Frontal rainfall

Slide 17 - Question de remorquage

An unequal distribution
Precipitation per year:

  • Tropics: 2000 mm
  • Desert: 250 mm 

Slide 18 - Diapositive

Learning goals
  • You understand how relief rainfall, convectional rainfall and frontal rainfall are being formed
  • You can point out the regions with high and low precipitation on a map 

Slide 19 - Diapositive

Today
  • Recap previous lesson
  • Explanation §3.4
  • Assignments workbook

Slide 20 - Diapositive

Start homework
  • Read §3.4
  • Make assignment 4, 5, 6 and 7

Finished?
Have the assignments checked by the teacher 

Slide 21 - Diapositive