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3.1 Water in motion
Today
WATER IN MOTION
What's the point? (5 min.)
Explanation 3.1 (10 min.)
Work on assignments (12 min.)
Check assignments (8 min.)
Work on summary (20 min.)
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Aardrijkskunde
Middelbare school
vwo
Leerjaar 2
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Today
WATER IN MOTION
What's the point? (5 min.)
Explanation 3.1 (10 min.)
Work on assignments (12 min.)
Check assignments (8 min.)
Work on summary (20 min.)
Slide 1 - Diapositive
What's the point?
Slide 2 - Diapositive
What's the point?
Responsibility of decisionmaking
Make sustainable choices
Slide 3 - Diapositive
Learning objectives 3.1
You can explain how the short and long hydrological cycles work.
You can tell in which forms water can be stored.
You can explain why a lot of water is unsuitable or unreachable for humans.
You can distinguish areas on the map of the world which are (too) dry or (too) wet.
Slide 4 - Diapositive
The journey of water: Water cycle
Short cycle: Water stays in more or less the same location.
Long cycle: Water goes on a big journey.
Forms of water:
Liquid (like rain)
Solid (like ice)
Gas (like water vapour)
Slide 5 - Diapositive
The journey of water: Water cycle
Which cycle is most important to us and why?
(Think about where we get our drinking water from.)
Slide 6 - Diapositive
The journey of water: Water cycle
Which cycle is most important to us and why?
The long cycle is most important to us, because with the short cycle fresh water (=zoet water) remains out of man's reach.
Slide 7 - Diapositive
Distribution of water
TERMS
Fresh water
versus
salt water
.
Surface water
versus
groundwater
.
#You can tell in which forms water can be stored.
#You can explain why a lot of water is unsuitable or unreachable for humans.
Skills: Why is it not a good figure?
Slide 8 - Diapositive
What happens with the ice?
Potential impact on sealevel?
Enough ice to make the sealevel rise 56 meter!
Potential impact on sealevel?
Only the ice on Greenland could make the sealevel rise. Impact relatively small.
Sea ice does not make the sealevel rise. Think about your drink with ice cubes, it does not overflow when the cubes melt.
Slide 9 - Diapositive
Where does the water go?
Accessible fresh water is scarce: we have to use it sparingly.
However a lot of precipitation flows back to the sea ‘unused’ because it:
falls in sparsely populated areas
only falls for a short period
falls in the winter when it is too cold to do arable farming (end of growing season)
Slide 10 - Diapositive
You can distinguish areas on the map of the world which are (too) dry or (too) wet.
Slide 11 - Diapositive
You can distinguish areas on the map of the world which are (too) dry or (too) wet.
Slide 12 - Diapositive
You can distinguish areas on the map of the world which are (too) dry or (too) wet.
Slide 13 - Diapositive
Get to work
3.1 (page 68 and 69 of the workbook): 2, 3, 4 and 5.
Question 5d: fallow = braakliggend = leegstaand/onbegroeid land
timer
12:00
Slide 14 - Diapositive
Check the assignments
3: A, C
4: B
5: E glacial river - rain river
F growing season - hibernation
Slide 15 - Diapositive
New approach
Before
the lesson you prepare a summary of the paragraph (in Dutch).
After
the lesson you change your summary when needed and then you hand in your summary. Extra challenge: rewrite your summary in English.
I will check your summaries and comment on it during the next lesson.
Slide 16 - Diapositive
Make a summary
Make a summary of paragraph 3.1:
Use your own words! Write in Dutch.
Use all terms.
Answer the learning goals.
Not too short nor too long - aim for about 20-25% of the total text.
Submit your summary via SOM.
Homework next week: Summary paragraph 3.2.
Slide 17 - Diapositive
Learning objectives 3.1
You can explain how the short and long hydrological cycles work.
You can tell in which forms water can be stored.
You can explain why a lot of water is unsuitable or unreachable for humans.
You can distinguish areas on the map of the world which are (too) dry or (too) wet.
Slide 18 - Diapositive
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