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characteristics of storms
develop between 5 and 30 latitude north and south of the equator
the sea temperature has to be 27 or higher
process of storm
the warm surface water evaporates, rises and condenses into clouds - this releases energy for storms
prevailing winds move the storm
the storm spins because of the coriolis effect
as the storm moves over the warm water the energy from it strengthens it - wind speed increases
storms lose energy when they go over cooler waters
eye of the storm
centre of the storm
up to 50km across and caused by descending air
low pressure, light winds, no clouds, no rain and high temperatures
eye wall
surrounds the eye
very strong winds
torrential rain
low temperatures
edges of the storm
wind speed falls
clouds become smaller and more scattered
rain becomes less intense
temperature increases