standard grade depressions john smith invergordon academy
TRANSCRIPT
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STANDARD GRADEDEPRESSIONS
John Smith Invergordon Academy
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LOW PRESSURE SYSTEMS
How depressions form
What happens at the warm front?
What happens at the cold front?
What happens in the warm sector?
What happens at the occluded front?
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Imagine an area out in the North Atlantic Ocean, to the West of the UK where the air is fairly cool.
Cold air will be shown in darker blue.
Warm air will be shown in red.
This cool air is represented by the light blue background on the following slides.
LOW PRESSURE SYSTEMS
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1. Cold Arctic air blowing from the North East
2. Warm moist Tropical air blowing from the South West
Imagine you are looking down on a large area of the North Atlantic Ocean. The air is quite cool (light blue).
THE AIRMASSES OVER THE ATLANTIC
In this area, different types of air masses meet. We will look at two of these.
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Cold Arctic air blows from the North East
Warm, moist Tropical air blows from the South West
THE AIRMASSES MEET……
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The two sets of air do not mix together
As they blow past each other, friction causes them to swirl round
……BUT THEY DO NOT MIX
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This means that we now have a cool area (shown by the light blue background)….…with a wedge of very cold Arctic air (shown by the darker blue triangle)….
There is also a wedge of warm moist Tropical air.
(red triangle)...
Warm, moist Tropical air
Cold Arctic air
…this is called the COLD SECTOR.
…this is called the WARM SECTOR.
WARM AND COLD SECTORS
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These systems usually move either East, or North East
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
DIRECTION OF MOVEMENT
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The line between the cooler air and the warm sector is called the WARM FRONT.
The line between the warm sector and the cold sector is called the COLD FRONT.
Cool air
Warm, moist Tropical air
Cold Arctic air
WARM AND COLD FRONTS
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Dense cool air
A SIMPLE CROSS SECTION THROUGH A DEPRESSION
COLD SECTOR
(cold, dense air) W A R M F R O N T
C O L D F
R O N T
THE WARM SECTOR
(warm, moist air)
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Warm, moist Tropical air
Cold Arctic air X
What conditions would be felt at X?
a) Cool
b) Cold
c) Warm
CONDITIONS AT STATION X (1)
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Warm, moist Tropical air
Cold Arctic air
What has passed over X?
a) Warm Front
b) Western Front
c) Cold Front
What conditions would be felt at X?
a) Cool
b) Cold
c) Warm
From which way are the winds blowing at X?
a) South East
b) North West
c) South West
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
X
CONDITIONS AT STATION X (2)
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What has passed over X?
a) Warm Front
b) Western Front
c) Cold Front
Warm, moist Tropical air
Cold Arctic air
From which way are the winds blowing at X?
a) North East
b) North West
c) South West
What conditions would be felt at X?
a) Cool
b) Cold
c) Warm Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
Warm, moist Tropical air
Cold Arctic air
X
CONDITIONS AT STATION X (3)
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WHAT HAVE YOU LEARNED SO FAR?
Warm moist Tropical winds blow from the South West
Cold Arctic winds blow from the North East
The wedge of warm air is called the warm sector
The wedge of cold air is called the cold sector
The leading edge of the warm sector is the warm front
The leading edge of the cold sector is the cold front
Low pressure systems are also called depressions
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WHAT HAPPENS AT THE WARM FRONT?
Warm air begins to rise over the cooler air
As this air rises, it begins to cool
Cool air can hold less water vapour than warm airWater vapour begins to condense into water dropletsWater droplets begin to form clouds
The first – and highest – type of cloud to form along the warm front is called Cirrus
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As the warm air rises, it cools.
Dense cool air
Warm air is forced to rise over denser, cool air.
Water vapour condenses and forms clouds
These high-level wispy clouds are called CIRRUS
AIR RISING ALONG THE WARM FRONT (1)
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CIRRUS CLOUDS
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Dense cool air
More moist air rises and cools
Clouds form lower down, and give prolonged rain
CIRRUS
PRECIPITATION AT THE WARM FRONT
These are CUMULUS
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CUMULUS CLOUDS
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Dense cool air
More moist air rises over the cooler air. As it does so it cools.
CIRRUS are very high and wispy. They are usually the first clouds we see as the warm front approaches
THE WARM FRONT - SUMMARY
CUMULUS clouds bring prolonged rain at the warm front
Warm
Front
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AN APPROACHING WARM FRONT
CIRRUS
CUMULUS
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WHAT HAPPENS AT THE COLD FRONT?
The cold Arctic air moves faster than the warm air.
The cold Arctic air is denser than the warm air.
The cold Arctic air undercuts the warm air, forcing it up. Water vapour begins to condense into water droplets
Water droplets begin to form very tall clouds
The clouds along the cold front are called Cumulonimbus.
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THE COLD FRONT
The cold front rapidly undercuts the air in the warm sector, making it rise very quickly.
The Warm Sector(warm, moist air)
The Cold Sector( cold dense air )
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Very tall clouds are formed by the rapidly rising air.
These are called CUMULONIMBUS.
The Warm Sector(warm, moist air)
CUMULONIMBUS give very heavy showers, sometimes with thunder and lightning.
PRECIPITATION AT THE COLD FRONT
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CUMULONIMBUS CLOUDS
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IN THE WARM SECTOR
Warm, moist winds blow from the South WestAir is forced to rise over cooler air
Condensation occurs, and forms Stratus clouds
Showers are common
The sky is very overcast
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Dense cool air
THE WARM SECTOR
Warm front
Warm, moist air in the warm sector is rising.
Cold Sectorcold dense air
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Dense cool air
CLOUD & PRECIPITATION IN THE WARM SECTOR
W A R M F R O N T
Warm, moist air in the warm sector is rising.
The clouds formed here are mostly Stratus
Stratus are flat layer clouds. They give showers.
STRATUS
Cold Sectorcold dense air
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CLOUD & PRECIPITATION – SUMMARY 1
Dense cool air
STRATUS
CIRRUSCUMULUS
CUMULONIMBUS
W A R M F R O N T
PERSISTENT RAINLIGHT SHOWERSHEAVY SHOWERS
Cold Sectorcold dense air
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A SATELLITE IMAGE OF A DEPRESSION
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CLOUD
PRECIPITATION
TEMPERATURE
WIND DIRECTION
AIR PRESSURE
Cumulonimbus
Stratus Cumulus Cirrus
Heavy showers
Showers Prolonged rain
Cold Warm
N.W. or N S.W. E or N.E.
CROSS SECTION THROUGH A DEPRESSION
FallingLowRising
Cool