3 - Climate factors

Welcome to geography!
Bilingual Education year 2




Mister De Graaf
Boss of Geography
1 / 27
volgende
Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 2

In deze les zitten 27 slides, met tekstslides.

Onderdelen in deze les

Welcome to geography!
Bilingual Education year 2




Mister De Graaf
Boss of Geography

Slide 1 - Tekstslide

Learning objectives
At the end of this chapter, you will be able to
• Explain the difference between weather and climate
• Describe the water cycle step by step
• Describe how three different types of rainfall are formed
• Explain climate differences between places
• Connect climate graphs to climate zones and places
• Describe and identify the different climate zones


Slide 2 - Tekstslide

This lesson
Reflection on last week (rainfall)
Homework discussion
Climate factors
Excercise

!NEW! - Learning objective - !EPIC! !MUST LEARN! - WOW!
Explain climate differences between places

Slide 3 - Tekstslide

Reflection

Slide 4 - Tekstslide

Reflection

Slide 5 - Tekstslide

Reflection

Slide 6 - Tekstslide

Reflection

Slide 7 - Tekstslide

The British Isles
Homework!

Slide 8 - Tekstslide

Your turn!
Write a description about precipitation on the British Isles (minimum 50 words)

Use the following words:
evaporates / prevailing wind / southwestern wind / mountains / condensation / wet / rain shadow

Homework!

Slide 9 - Tekstslide

Your turn!
Water in the ocean evaporates, due to the heat of the sun. The prevailing wind on the British Isles comes from the southwest. We call this a southwestern wind. The wind blows the moist air against the mountains. When the moist air climbs, it cools down and there will be condensation. This will lead to wet weather on the southwest side of the mountains. The northeastern part of the mountain will stay dry, we call this the rain shadow.


Homework!

Slide 10 - Tekstslide

Climate factors

Slide 11 - Tekstslide

#1 Latitude
Rule #1: How further from the Equator, how colder
(or: the higher the latitude, the colder)

Slide 12 - Tekstslide

#1 Latitude

Slide 13 - Tekstslide

#2 Altitude
Rule #2:  how higher, how colder

Slide 14 - Tekstslide

#2 Altitude
Sunlight doesn’t provide warmth right away (otherwise it would be really warm out in space!)
When the sunlight hits the earth, it’s reflected as warmth
From there the warm air rises and slowly cools
So the higher you go, the colder it gets!

Slide 15 - Tekstslide

#2 Altitude
Sunlight doesn’t provide warmth right away (otherwise it would be really warm out in space!)
When the sunlight hits the earth, it’s reflected as warmth
From there the warm air rises and slowly cools
So the higher you go, the colder it gets!

Slide 16 - Tekstslide

Slide 17 - Tekstslide

#3 Ocean currents
Rule #3: How further away from warm ocean currents, how colder (its winter)

Slide 18 - Tekstslide

Slide 19 - Tekstslide

#4 Distance from the coast 
Rule #4: The closer to the coast, the smaller the difference between summer and winter temperature.

Slide 20 - Tekstslide

The summer temperature is cooled by the sea
The winter temperature is warmed by the sea
Reflection

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Slide 22 - Tekstslide

#5 Prevailing wind direction
Rule #5: Dependent on its direction, wind can carry either warm or cold air and can either carry dry or moist air

Slide 23 - Tekstslide

Summarised
The following factors influence a place’s climate
(temperature and precipitation that is):
  1. Latitude (distance from the Equator)
  2. Altitude (height)
  3. Ocean currents
  4. Distance from the coast
  5. Prevailing wind direction

Slide 24 - Tekstslide

What to do
Revise your homework

Agenda:
Small Test October 17th - Theory in studiewijzer Magister + notes


Slide 25 - Tekstslide

5 main climate regions
  1. Equatorial climates​ (or tropical climates)​
  2.  Arid climates​ (or dry climates)​
  3.  Maritime climates​ (or sea climates)​
  4.  Continental climates​ (or land climates)​
  5.  Polar climates​ (incl. mountain climates)​




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Slide 27 - Tekstslide