In deze les zitten 28 slides, met tekstslides en 2 videos.
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Chapter 1: U.S.
§1.2 Extreme weather
Slide 1 - Tekstslide
Learning objectives through these questions:
What is air pressure?
Which types of air masses are prevalent in the US?
Which weather extremes can occur as a result of these air types?
How does a tornado form?
Slide 2 - Tekstslide
What is air pressure?
Air pressure: The weight of the air pressing down on the earth.
Measure with:
-barometer
-unit: hectopascal (hPa) or millibar (Mb)
Slide 3 - Tekstslide
High pressure
High pressure = falling air
This air is heavy
Symbol on the map = H
Pressure: around 1020 hPa
Which weather type belongs to H?
- no clouds
- dry
- why?
Slide 4 - Tekstslide
High pressure
High pressure = falling air
This air is heavy
Symbol on the map = H
Pressure: around 1020 hPa
Which weather type belongs to H?
- no clouds
- dry
- falling air warms up near earth surface, clouds dissolve, clear skies
Slide 5 - Tekstslide
Low pressure
Low pressure = rising air
the weight of that air is low
Symbol on the map = L
pressure: around 1000 hPa
Which weather type belongs to L?
- clouds
- precipitation
- why?
Slide 6 - Tekstslide
Low pressure
Low pressure = rising air
the weight of that air is low
Symbol on the map = L
pressure: around 1000 hPa
Which weather type belongs to L?
- clouds
- precipitation
- (moist) air rises, air cools down, condensation takes place (cold air holds less moisture than warm air)
Slide 7 - Tekstslide
Air moves
Air moves due to a difference in air pressure, from high pressure areas to low pressure areas
Slide 8 - Tekstslide
Influence of air pressure on the weather
Example California:High pressure area in summer -> dry and sunny weather (Mediterranean climate)
In winter: more western winds, bringing rain
L
Slide 9 - Tekstslide
4 basic types of air masses:
moist -> above sea
dry -> above land
cold -> in the north
warm -> in the south
where 2 different types of air masses collide: front
At fronts, low pressure areas (depressions) can occur, causing extreme weather situations.
Air masses in the US:
Slide 10 - Tekstslide
Air types and their effect
(Collision of) air types have a major influence on the weather in the US.
Which 3 air types in the picture cause the following examples of extreme weather? Why only those 3?
Northerns (cold wave)
Southerns (heat wave)
Tornadoes
Hurricanes
Front
<span style="font-weight: bold">Front</span> = grensgebied tussen twee verschillende luchtsoorten.<div>Op deze plek ontstaan depressies (lage druk) Vaak is het dan slecht weer.</div>
Slide 11 - Tekstslide
Slide 12 - Tekstslide
Slide 13 - Tekstslide
Tornadoes
Tornadoes occur where different types of air come together. Cold, dry air (Canada) collides with warm, moist air (Gulf of Mexico).
Slide 14 - Tekstslide
Slide 15 - Video
Formation tornadoes
Collision of dry cold air from the north with warm moist air from the south
Warm air rises quickly, rotating
Cold air descending, also rotating
A funnel cloud forms
Suction of surrounding air (works as a huge vacuum cleaner)
Forms during heavy thunderstorms with with large wind speed in the higher air layers
Slide 16 - Tekstslide
Tornadoes
Slide 17 - Tekstslide
Slide 18 - Tekstslide
Slide 19 - Tekstslide
Characteristics tornadoes
Tornadoes form in the spring
Location unpredictable (as opposed to hurricanes)
They form on land (as opposed to hurricanes)
Tornadoes are small in size (local phenomenon): < 1 km diameter
Higher wind speeds than hurricanes: 100 - 400 km/hour
There are more tornadoes than hurricanes per year in the US (around 1000 per year)
Slide 20 - Tekstslide
Slide 21 - Video
Slide 22 - Tekstslide
Formation of a hurricane (1:40 min.)
Slide 23 - Tekstslide
Formation of a hurricane
Temperature sea water minimum of 26 / 27 degrees Celsius causing high levels of evaporation
Warm, moist are rises, cools down and condensates --> high amounts of rainfall
Energy (warmth) is released through condensation --> extra rising air
Surrounding air is being sucked in from surrounding area
Wind is rotating around the eye (calm weather, no clouds)
Slide 24 - Tekstslide
Slide 25 - Tekstslide
Characteristics hurricane
Forms above oceans
Until 500 kms in diameter; the eye is 20-50 km in diameter
Wind speeds up to 300 km/hour
Between June and November: the temperature of the sea water has to be warm enough (northern hemisphere)
Saffir-Simpson scale to indicate strength (1 - 5; 5 is highest category)
Slide 26 - Tekstslide
Het orkaangebied
orkaangebieden wereldwijd
<span style="font-weight: bold">hurricane </span>: Noord-Amerikaanse benaming voor 'orkaan'
<span style="font-weight: bold">tyfoon </span>: Aziatische benaming voor 'orkaan'
<span style="font-weight: bold">cycloon </span>: Afrikaanse benaming voor 'orkaan'
<span style="font-weight: bold">Willy-Willy </span>: Australische naam voor 'orkaan'