Weather Hazards Flashcards
Atmospheric circulation
Atmospheric circulation is Earth’s large-scale air movement, driven by solar energy, forming wind systems and cells (Hadley, Ferrel, Polar) to distribute heat and shape climates.
Degrees of the equator
0 degrees
5 steps of storm formation
- Warm moist air rises which leaves low pressure below. Causing warm air to move into this area and rise too.
- The air cools and condenses into thunderstorm clouds
- It spins clockwise in southern hemisphere and anti in northern hemisphere due to Coriolis effect
- The addition of energy speeds up the wind pushing it to 75 mph which is category 1 storm.
5.The storm develops an eye an area of low pressure and is relatively calm. Surrounding it is the eyewall whiich has the most intense winds and storms.
Storm surge
When a tropical storm picks up lots of water and pushes it onto the coast.
How does a storm dissipate
WHen they reach nearer to land as the water is their energy source.
How do tropical storms form
Temperature- Must be 26-27 degrees and 50 metres deep as water needs a lot of energy to heat up.
Air pressure-Areas of unstable pressure where low and high pressures meet so that warm air rises more readily and clouds can form.
Wind speed- Winds must be present but not too strong or they will rip the storm apart
Rotation- They form only 5-30 degrees of the equator. But not on the equator due to the Coriolis effect.
What are tropical storms called
Hurricane
Cyclone
Typhoon
Tropical storm
A stotm that is created in the tropics
Different types of wind
Trade Winds: Blow from 30° N/S to the equator, curving due to Earth’s rotation.
Westerlies: Blow from 30° N/S to 60° N/S, also curving.
Polar Easterlies: Blow from the poles to 60° N/S.
Coriolis effect
The Coriolis effect makes winds curve because of Earth’s rotation. In the Northern Hemisphere, they curve right; in the Southern Hemisphere, they curve left.
Polar cell
The Polar cell, the smallest atmospheric cell, spans 60° to 90° latitude. Cold air sinks at the poles, creating high pressure. It flows south, warms, rises, and cycles back.
Ferrel Cell
The Ferrel cell, the middle cell, spans 30° to 60° latitude. It moves opposite to Hadley and Polar cells, like a cog. Air sinks from the Hadley cell, travels to mid-latitudes, rises near Polar cell air, and causes unsettled weather, especially in places like the UK.
Hadley Cell
The Hadley cell, the largest atmospheric cell, spans the equator to 30°-40° latitude. Warm air rises at the equator, forming storms, then cools and sinks over subtropics, creating dry, warm climates where deserts are common.
Why is the equator hot
Due to the curvature of the earth and the rays of sunlight concentrate on the centre where the equator is. Further from this are the poles which are the coldest places on earth.
Draw the angle of insolation