3.6 Polar climates

3.6 Polar climates
1 / 16
volgende
Slide 1: Tekstslide
AardrijkskundeMiddelbare schoolhavo, vwoLeerjaar 3

In deze les zitten 16 slides, met interactieve quizzen, tekstslides en 1 video.

time-iconLesduur is: 30 min

Onderdelen in deze les

3.6 Polar climates

Slide 1 - Tekstslide

Learning objectives
After studying this section, you will be able to:
  • Describe the polar climates
  • Explain the location of the polar climates

Slide 2 - Tekstslide

Polar climates and landscapes
Three types of polar climate?

Slide 3 - Tekstslide

Polar climates and landscapes
Three types of polar climate?
  • Tundra climate (ET)
  • Ice cap climates (EF) > high latitude
  • Mountain ranges (EH) > high altitudes

Slide 4 - Tekstslide

Polar climates and landscapes
Tundra climate: at least one month in which the temperatures are higher than 0 °C, but none of the months is warmer than 10 °C. 

Ice cap climate: the temperature never exceeds 0 °C. 

The tundra climate does experience precipitation, but the ice cap climate is quite arid.

Slide 5 - Tekstslide

The tundra climate 

Slide 6 - Tekstslide

A tundra pond in the summer months - surface snow melts, forming a freshwater pond.

Slide 7 - Tekstslide

The ice cap climate

Slide 8 - Tekstslide

Which climate does the graph show?
A
Tundra climate (ET)
B
Ice cap climate (EF)

Slide 9 - Quizvraag

Which climate does the graph show?
A
Tundra climate (ET)
B
Ice cap climate (EF)

Slide 10 - Quizvraag

Which climate does the graph show?
A
Tundra climate (ET)
B
Ice cap climate (EF)

Slide 11 - Quizvraag

Tundra climate (ET)
Ice cap climate (EF or EH)

Slide 12 - Tekstslide

The Albedo Effect
The Earth’s albedo, or reflectivity, is another reason why temperatures in the polar regions are low: white snow is a good reflector of sunlight, so not much gets absorbed. As a result, the temperature in the region does not increase significantly when sunlight does reach the polar region in the summer season.

Slide 13 - Tekstslide

Slide 14 - Video

Slide 15 - Link

The changing polar climate
  • Temperatures in the Arctic and Antarctic are increasing faster than in other regions.

  • Effect on a regional scale: melting permafrost > buildings that were built on the once frozen soil have slowly started sinking

  • On a global scale, melting permafrost impacts the climate

Slide 16 - Tekstslide