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3 tto part II
First 10 minutes: Work on your own!
- Read section 3.1 and read your notes from last time!
- Unfortunately don't have the test results, but before the end of the lesson you might have! You will correct your own test :D
- I need to do something important, I will tell you later
- Ten minutes later we will continue!
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Slide 1:
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Aardrijkskunde
Middelbare school
havo, vwo
Leerjaar 3
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First 10 minutes: Work on your own!
- Read section 3.1 and read your notes from last time!
- Unfortunately don't have the test results, but before the end of the lesson you might have! You will correct your own test :D
- I need to do something important, I will tell you later
- Ten minutes later we will continue!
Slide 1 - Diapositive
Planning:
Reading and answering questions
Recap last time
El Nino
Lesson goals
which factors influence the climate
What is el Nino and what are the differences between el Nino situation and the normal situation?
Slide 2 - Diapositive
Why doesn't the seawater off the coast of Chile evaporate.
A
The seawater is too warm so it does not evaporate
B
The seawater is too salty and does not evaporate
C
The seawater is too cold so it does not evaporate
Slide 3 - Quiz
How many climates does Chile have?
A
3
B
4
C
5
D
6
Slide 4 - Quiz
In a high-pressure area it does not rain because the air sinks. Why is that?
A
Rain only occurs when air becomes colder and descending air becomes warmer
B
Rain only falls when there is moisture in the air and valley air is dry
C
Rain only falls when there is a lot of wind and when the air is falling it does not blow
D
Rain only falls when there are clouds and descending air is too dry for tha
Slide 5 - Quiz
What is not a reason why the north of Chile is so dry?
A
The cold Humboldt current provides cold seawater
B
It is located on the leeward side of the Andes
C
High pressure causes air to descend
D
It's a desert. Duh
Slide 6 - Quiz
Instruction/make notes!
Slide 7 - Diapositive
e
Slide 8 - Diapositive
Temperature factors
Latitude: the further from the equator, the colder.
Altitude: the higher, the colder.
Location in relation to the sea: the further from the sea, the warmer in summer and the colder in winter.
Supply of cold or heat from elsewhere by wind or sea currents.
Location of mountains: sheltered or not.
Slide 9 - Diapositive
Arid conditions in Chile
Combination of three factors:
High-pressure area
Humboldt currents (ocean current)
the Andes Mountains
Slide 10 - Diapositive
Droogte in Chili
(Atacama woestijn)
Droogte komt door:
Subtropisch hogedrukgebied
Humboldtstroom (zeestroom)
Het andesgebergte
Slide 11 - Diapositive
High-pressure area
1. high-pressure area
Slide 12 - Diapositive
Humboldt current
Slide 13 - Diapositive
3. Andesmountains
Slide 14 - Diapositive
EL NIÑO
Read El Nino in your coursebook on page 44
Slide 15 - Diapositive
Slide 16 - Diapositive
Slide 17 - Vidéo
5. Ocean currents
Warm current -> warmer air
Cold current -> colder air
Slide 18 - Diapositive
Slide 19 - Diapositive
Slide 20 - Diapositive
www.bnnvara.nl
Slide 21 - Lien
El Niño (het jongetje)
Opwarming zeewater door omgedraaide lucht- en zeestromen
Warmer zeewater:
Minder vissen
meer verdamping > meer neerslag, overstromingen etc>
Slide 22 - Diapositive
Het Kerstkind
El Niño
- Verandering in lucht- en zeestromen (rond kerstmis). - Gevolgen voor Chili: warmer zeewater, meer neerslag, overstromingen, minder visvangst.
Slide 23 - Diapositive
Slide 24 - Vidéo
Slide 25 - Vidéo
Work, work, work
Read section 1: 3 climate Chile
complete assignments 1 to 9
use:
Textbook pages 44/45
Homework for Thursday 7/11
Next lesson: Explanation of Christmas child El Niño!
Last few minutes of this lesson: 4 questions!
Slide 26 - Diapositive
herhalen/nabespreken
Slide 27 - Diapositive
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