The world's major winds that revolve from temperature differences
How wind is created
1. Air is heated, it expands and rises
2. Air cools, it contracts and sinks
3. Difference in pressure causes wind to blow from high to low pressure
Air circulation
Air rises at equator, flows to poles, cools and sinks at outer tropics, returns along surface to equator
Doldrums
Low-pressure region at equator where air is hot and rising
Poles
High-pressure region where air is cold and heavy, sinking and diverging towards equator
Movement of winds in low pressure
Winds deflected to the right in northern hemisphere (Ferrel's low)
Movement of winds in high pressure
Winds move outward from center (northern hemisphere)
Air pressure or atmospheric pressure
Caused by the weight of the air pressing on the Earth's surface
The atmosphere exerts a pressure of about one kilogram on each square centimetre of the Earth's surface
Air pressure
Measured in millibars (mb)
Average air pressure at sea level is about 1013.25 mb
Atmospheric pressure
Measured by an instrument called a barometer
Types of barometers
Mercury barometer
Aneroid barometer
Mercury barometer
Consists of a graduated, straight glass tube or column, with one end sealed and filled with mercury, with the open end standing in a small vessel containing more mercury
Height of the column of mercury
Can be read against a vertical scale to indicate the pressure of the air
Plotting data about atmospheric pressure on weather maps
Using isobars, which are lines on the map that join all the places with the same atmospheric pressure
Winds that blow frequently from one direction, such as the Trade Winds, are called prevailing winds
The Trade Winds are confined to areas 5 to 30 degrees north and south of the equator
The Trade Winds create pleasant temperatures that are popular with tourists, which is one reason why the Caribbean is such a popular and attractive tourist destination
Where trade winds converge
Along a line called the Inter-Tropical Convergence Zone (ITCZ), an area of low pressure lying along the equator
Easterly waves
Troughs of low pressure moving across the Atlantic and Caribbean on the southern fringes of the ITCZ, prevailing from May to November and associated with showers and thunderstorms
Hurricanes
Intense, tropical or cyclonic storms in which the winds move in a spiral fashion, with speeds of over 120 kilometres per hour
Hurricanes develop in the Mid-Atlantic Ocean between latitudes 5°N and 20°N
Hurricanes generally move in a north-westerly direction in the Caribbean
Hurricanes are prevalent in the Caribbean and the Gulf of Mexico from June to November and are associated with torrential rainfall and thunderstorms
Pressure in hurricanes
Low, with winds blowing inwards in an anti-clockwise direction
Eye of the hurricane
An area of calm at the centre of the hurricane, with heavy rainfall occurring around it
Hurricanes are very destructive, damaging lives, property and crops, and causing large tidal waves and flooding along coastal areas in the hurricane's path
Tornado
A small, violent, tropical storm prevalent in Florida and other parts of the USA
Many people think hurricanes are connected to global warming, which is caused by the increased carbon dioxide in the atmosphere
The theory of global warming is supported by the evidence of increased sea temperatures and rising sea levels, such as the erosion of beaches in the Dominican Republic