Cette leçon contient 27 diapositives, avec quiz interactif, diapositives de texte et 6 vidéos.
La durée de la leçon est: 45 min
Éléments de cette leçon
Wind systems
Repeating the material
Slide 1 - Diapositive
Energy Balance
Get your notebook or a piece of paper.
Slide 2 - Diapositive
Slide 3 - Diapositive
Coördinaten
Om een locatie te kunnen aanwijzen heb je twee getallen nodig: de breedtegraad en de lengtegraad (longitude.
Longitude
Latitude
Slide 4 - Diapositive
Where is an energy surplus?
A
Low latitude
B
Middle latitude
C
High latitude
Slide 5 - Quiz
Is an energy surplus a positive or a negative thing?
Slide 6 - Diapositive
Negative
Enhanced greenhouse effect
Positive
Renewable energy --> Solar Panels
Slide 7 - Diapositive
What is the difference between an energy deficit and an energy surplus?
Slide 8 - Diapositive
Energy deficit (Low) Less energy than needed. More outgoing than incoming energy
Energy surplus (High)
More energy than needed.
More incoming than outgoing energy.
Slide 9 - Diapositive
Global warming
Global warming is caused by the enhanced greenhouse effect. The greenhouse gases reflects heat coming from the surface of the earth back towards the earth. This causes the atmosphere to increase in temperature
Slide 10 - Diapositive
Slide 11 - Diapositive
Slide 12 - Vidéo
Slide 13 - Vidéo
Slide 14 - Vidéo
Temperatures above land and sea
Slide 15 - Diapositive
Land gets warmer than water but it gets colder than water too.
Land heats up and cools down faster than water.
Slide 16 - Diapositive
What effect does this have on for example the Netherlands?
Slide 17 - Diapositive
In coastal areas, temperature differences are small.
(Flora and Fauna)
Slide 18 - Diapositive
Pressure: High pressure & Low pressure
Slide 19 - Diapositive
Slide 20 - Vidéo
High pressure area
Sinking air due to low temperatures.
Summer: Hot & Dry Winter: V Cold & Dry
+ / H / Maximum
Air molecules are close to eachother --> heavy --> sinking
Slide 21 - Diapositive
Low pressure area
Rising air due to high temperatures.
Summer: Hot & Rain Winter: Cold & Snow
- / L / Minimum
Air molecules are further away from eachother --> not as heavy --> rising
Slide 22 - Diapositive
Slide 23 - Vidéo
Global wind patterns
Slide 24 - Diapositive
What is Buys Ballot's Law?
Slide 25 - Diapositive
1. Air moves from H --> L
2. In the northern hemisphere the wind has a deviation to the right, in the southern hemisphere a deviation to the left (as if the wind is in your back when you're standing on the equator).