Chapter 7.3 Talas rages over Japan (part 2)

Chapter 7.3
Talas rages over Japan (part 2)
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Chapter 7.3
Talas rages over Japan (part 2)

Slide 1 - Tekstslide

The aims of this paragraphe
Things you should know:
  • how hurricanes affect people, the economy and the landscape
  • the characteristics of a hurricane
  • the relationship between levels of development and the damage and number of victims caused by hurricanes
  • how to classify a hurricane according to the Saffir-Simpson scale (figure 12)



Slide 2 - Tekstslide

G8 Dimensions
Look at an area in different ways:
● The physical dimension is about natural subjects such as climate or soil.
● The economic dimension is about earning money and employment.
● The socio-cultural dimension has to do with languages, religions, living conditions and other characteristics of the inhabitants.
● The demographic dimension is about the changes in population size.
● The political dimension is about who is in charge, for example the influence of a ministry or interest group.



Slide 3 - Tekstslide

G52 Wind
The air around us consists of billions of small particles (molecules).
The moving mass of air is called wind. When the air moves quickly, the wind force is high. 
You can measure wind speed with a wind meter. 
When the wind speed reaches 12, there is a hurricane. The Beaufort scale is still used in weather forecasts.

Slide 4 - Tekstslide

G57 and G58 Hurricanes
A hurricane is a heavy tropical storm with a wind force of at least 12 on the Beaufort scale. The storm forms above seawater with temperatures above 26.5°C. 
These high temperatures only 
occur at the end of summer.

Slide 5 - Tekstslide

Other characteristics
  • Hurricanes are between 500 and 1,500 km wide. 
  • A hurricane lasts between five and ten days on average.
  • Hurricanes occur mainly in the tropics.
  • Every tropical storm is given a name.
  •  The wind can reach speeds of between 100 and 250 km per hour.
  • A hurricane consists of a circular low-pressure area that rotates around an eye

Slide 6 - Tekstslide

1
Hurricanes form above warm seawater (at least 26.5°C.)
The air above the sea is warm and a lot of seawater has evaporated. 
2
Moist air rises quickly, cools down, and then it starts to rain.
3
As the water vapour condenses, heat is released, which makes the air rise even more quickly. 
4
The low pressure at sea level causes air to be sucked in from all directions. (like a vacuum-cleaner)

Slide 7 - Tekstslide

September 2020

Slide 8 - Tekstslide

The wind direction and sea currents are heading in the same direction

Slide 9 - Tekstslide

Slide 10 - Video

Slide 11 - Link

Is there a relationship between hurricanes and human action? 

Slide 12 - Tekstslide

Learn chapter 7.3 and do assignment 1-2-3-4 on the geo online.

Slide 13 - Tekstslide