Tropical storms are areas of low pressure with winds moving in a spiral
They last days to weeks and have speeds over 74mph over warm water (>27 degrees)
Tropical storms are measured by the Saffir-Simpson scale, which categorizes them from 1-5 based on sustained wind speed and estimates potential property damage
Tropical storms form from the equatorial regions 30N and S above the equator between the tropics of Cancer and Capricorn
Global circulation is a world-wide system of winds that transport heat from tropical to polar latitudes
Differential heating causes air expansion and changes in pressure, leading to wind as a result of pressure changes in the atmosphere
High temperatures at the equator cause air to rise, creating low pressure, while air cools and sinks at around 20-30 degrees leading to high pressure
The spin of the earth induces the Coriolis effect in the Northern hemisphere, causing winds to curve
When the Hadley cell is complete, the air flows back to the equator as trade winds
Hurricanes rotate counterclockwise in the Northern hemisphere due to the Coriolis effect
Conditions for storms to form include sea temps >27 degrees, ocean depth of >70m, location between 5-20 degrees North and South, low level convergence of air, and rapid outflow of air in the upper atmosphere
Hurricanes begin as thunderstorms and develop from warm, moist air rising to create low pressure
The eye of a hurricane is an area of extremely low pressure surrounded by a spinning vortex of high winds and heavy rain
Tropical storms form in the Northern Hemisphere from June-November and in the Southern Hemisphere from November-April
Hazards caused by tropical storms include high winds, flooding, landslides, and storm surges