Depressions Flashcards
What are depressions
Low pressure weather systems- areas of low atmospheric pressure, often below 1,000 mb
How are depressions represented on a weather map
A system of closed isobars with pressures decreasing towards the centre
Where do depressions move
Rapidly from west to east across the British isles
What are the isobars of a depression like
Usually close together, producing a steep pressure gradient from the outer edges to the centre
Winds in a depression
Often strong and blow inwards towards the centre of the low in an anti-clockwise direction
When is the wind said to veer
In the Southern part of the British Isles, a change in wind direction occurs from south to southwest to west to northwest as the depression moves across from west to east
When is the wind said to back
In the northern parts of the British isles the wind changed direction from southeast to east to northeast to east
What are the two air masses involved in a depression affecting the British isles in the North Atlantic
- polar maritime air, which is dense, moist and cold
- tropical maritime air, which is light, moist and warm
What happens as the two bodies of air that form the depression above the British Isles move towards each other
The warmer, less dense air from the south rises above the colder, dense air from the north- the rising air is removed by strong upper atmospheric winds (the jet stream) , but as it rises the Earth’s rotational spin causes it to twist
= a wave at ground level in the polar front, it increases in size to become a depression
What two parts of the original front have developed after the two bodies of air have mixed and twisted
- the warm front at the leading edge of the depression where warm, less dense air rises over the colder air ahead
- the cold front at the rear of the depression where colder dense air pushes against the warmer air ahead
What lies between the warm front and the cold front
The warm sector
What is the warm sector
An area of warm and moist air
What is an occlusion
As the depression moves eastwards, the cold front gradually overtakes the warm front to form an occlusion in which the colder air undercuts the warmer air so that it no longer touches the ground