tropical storms Flashcards
define a tropical storm
A revolving low pressure system, bringing strong winds, rainfall and storm surges
- what happens towards the edges of the storm
towards the edges of the storm wind speed falls, the clouds become smaller and more scattered, the rain becomes less intense and the temperature increases
- what is the eye wall [
the eye is surrounded by the eyewall, where there’s spiralling rising air, very strong winds, storm clouds, torrential rain and a low temperature
- what is the centre of the storm called
the centre of the storm is called the eye- its up to 50 km across and is caused by descending air
theres very low pressure light winds, no clouds no rain and a high temperature in the eye
- what are the characteristics of a tropical storm
tropical storms are circular in shape, hundreds of kilometres wide and usually last 7-14 days. they spin anticlockwise in the nothern hemisphere and clockwise in the southern hemisphere
- describe the formation of a tropical storm
the warm surface water evaporates, rises, and condenses into clouds. this releases huge amounts of energy, producing powerful storms, the rising air creates an area of low pressure which increases surfaces winds. Low wind shear prevents clouds from breaking up as they rise, so the storm stays intact.
easterly winds near the equator move tropical storms to the west the storms spin because of the Coriolis effect as the storm moves over the ocean the energy from the warm water strengthens the storm, so wind speed increases. storms lose strength when they move over land or cooler water because the energy supply from the water is cut off
- how does global atmospheric circulation affect weather and climate
at the equator the son is directly overhead- this means the earths surface recieves a lot of solar radiation, so its hot. Warm, moist air rises and forms clouds, so it rains a lot
by the time air reaches 30 degrees north and south of the equator it has released most of its moisture as rain. the dry air means there are few clouds and little rainfall, so deserts are often found at this latitude The UK lies close to the low pressure zone at 60 degrees north. warm rising air brings lots of cloud cover and rainfall, often as low pressure systems carried from the atlantic by westerly wind
- how does air move in the three cells
the sun warms the earth at the equator, causing the air to rise. this creates a low-pressure belt.
as the air rises it cools and moves away from the equator 30 degrees north and south of the equator, the cool air sinks, creating a high-pressure belt at the ground surface, the cool air moves either back to the equator as trade winds or towards the poles as westerlies. this winds curve because of the earths rotation- this is called the coriolis effect 60 degrees north and south of the equator the warmer surface winds meet colder air from the poles. the warmer air rises to create low pressure some of the air moves back towards the equator, and the rest moves towards the poles at the poles, the cool air sinks, creating high pressure. The high-pressure air is then drawn back towards the equator
- what does each cell consist of
each cell has warm rising air that creates a low-pressure belt and cool sinking air that creates a high-pressure belt.
- what is the global atmospheric circulation system divided into
the global atmospheric circulation system is divided into cells
- why does air move
air moves due to differences in air pressure- winds blows from high pressure areas to low pressure areas
- what is global atmospheric circulation
global atmospheric circulation is the transfer of heat from the equator to the poles by the movement of air
Coriolis effect
The effect of Earth’s rotation on the direction of winds and currents.
Distribution of tropical storms
occur in tropical areas between 5 - 15 degrees north and south of the equator
Strongest are in the East Pacific - Japan / Philippines
none of coast of America due to cold currents
Conditions for tropical storms
- latitude between 5-20 N&S
- sea 26C or over
- heat sea to depth of 70m
- coriolis force
- low wind speeds at high altitudes