Everything You Need to Know About Hurricanes, Plus What to Expect in 2022

How do hurricanes develop? What conditions cause them to form—specifically, why do they need warm waters?

Hurricanes develop over warm tropical waters, primarily during the summer and fall. To develop, a hurricane needs:

1. Water temperatures of 27°C (80°F) or greater – Hurricanes are basically heat engines, in that they derive their energy from the release of latent heat in the condensation process. As warm, moist tropical air rises, it condenses into clouds and rain, releasing heat into the atmosphere. This heat results in more rising air, squalls (sudden violent gusts of wind), and a lowering of the surface pressure. As the surface pressure drops, air begins to flow towards the low pressure area. The Coriolis Effect causes this air to rotate (counter-clockwise in the Northern Hemisphere, clockwise in the Southern Hemisphere). Given other favorable conditions, the rotating area of squalls may become a tropical storm or hurricane.
   
   
2. Low wind shear – Hurricanes are very delicate structures in that they do not tolerate winds blowing at different speeds or different directions above the center (wind shear). To develop into a hurricane, the winds aloft need to blow from approximately the same direction and at the same speed. This gives the young disturbance time to build a vertical column of squalls.
   
   
3. Pre-existing disturbance – Hurricanes do not develop out of “thin air,” they require some type of pre-existing weather feature to initially focus the squalls. This feature could be a tropical wave, an area of low pressure that moves off the west coast of Africa and tracks across the tropics, or it could be residual squalls along the trailing end of a cold front that dips into the tropics.

How are hurricanes predicted? How early can we predict with accuracy? How can early prediction help businesses?

Data from around the world are fed into computer models, which use complex equations with many variables to predict weather patterns. Just as these models can predict the development of storm systems that bring rain or snow in the winter months, these same models can predict the development of low pressure areas in the tropics that can develop into hurricanes. However, accurately predicting the precise track of a hurricane days in advance remains a problem. The difficulty lies in obtaining accurate atmospheric data across the tropical oceans. Without direct observations, we must estimate what is happening at all levels of the atmosphere across the oceans. As with any computer program, bad or insufficient data will result in a poor forecast. This is why aircraft reconnaissance is so important: the more accurately we can define the initial conditions in the tropics, the better we can predict the path and intensity of a tropical cyclone.

Modern computer models can predict day-to-day weather as far as two weeks out. Often, they can pick up on potential tropical cyclone development 7-10 days in advance. This gives us the ability to initiate advisories on tropical disturbances days before they are classified as tropical depressions or tropical storms. In 2016, StormGeo initiated advisories on a disturbance in the eastern Atlantic nine days before it developed into Hurricane Hermine. This provided businesses in the eastern Caribbean Sea and the Gulf of Mexico time to prepare for the storm.

Why is the Gulf of Mexico prone to hurricanes?

The Gulf of Mexico is a body of very warm water that lies in the tropics, making it an ideal environment for hurricanes.

How is global warming affecting the amount, size or power of hurricanes?

There is no conclusive evidence that global warming is having any effect on hurricanes. Looking back over the past 100 years, there has been a definite increase in the number of hurricanes, however, this is likely due to better detection techniques. Prior to observing the Tropics with earth-orbiting satellites (the first weather satellite was launched in 1959) the knowledge of the existence of hurricanes and other tropical systems relied mainly upon the human eyes of those aboard ocean-going ships.

We now know with certainty that for the past 40 years, worldwide tropical cyclone activity has actually been declining. As for intensity, there are more strong hurricanes now than in the past. Again, this may be contributed to poor observations in the past. Without reconnaissance and satellite data, many strong hurricanes were likely missed prior to the mid 1900s. One thing we do know is that hurricane impacts along the U.S. coast have actually shown a slight decrease over the past 100 years.

Subtropical storm Andrea, May 2019

What is a subtropical storm?

A subtropical storm is a low pressure area that forms in the tropics or subtropics. The tropics are a region identified as the area north of the Equator to the Tropic of Cancer and south of the Equator to the Tropic of Capricorn. The subtropical regions are defined as areas extending approximately 12 degrees of latitude north and south of the tropics. Unlike a tropical storm, a subtropical storm typically does not have its strongest winds or heaviest squalls over the center. This makes it more difficult for the storm to strengthen. Want to learn more about subtropical and extratropical storms? Watch the explainer video. 

If hurricanes slow down, how does that make them more dangerous?

A slower-moving hurricane increases the amount of time that its strong winds impact a location. In addition, the amount of rainfall that a hurricane produces is directly related to its speed of movement. A rule of thumb meteorologists use to estimate rainfall is to divide the forward speed into 100. For example, a hurricane moving at 15 mph may produce 6-7 inches of rain, while one moving more slowly at 5 mph might generate 20 inches of rain. This is true for any tropical low-pressure area, not just hurricanes. Any tropical low can produce extremely heavy rainfall if it moves slowly across an area.

What is the difference between a tropical disturbance, tropical depression and tropical storm?

Tropical Disturbance: An area of squalls that may be associated with westward-moving low-pressure areas that move off the west coast of Africa in the summer months, or they may be associated with weak frontal boundaries that extend into the tropics or subtropics. There is no circulation center at the surface.

Tropical Depression: A low-pressure area over the tropical ocean that has a well-defined low-level circulation center along with organized squalls around the center. Winds are less than 39 mph.

Tropical Storm: A low-pressure area over the tropical ocean that has a well-defined low-level circulation center along with organized squalls around the center. Winds are 39-73 mph.

Hurricane: A low pressure area over the tropical ocean that has a well-defined low-level circulation center along with organized squalls around the center. Winds are 74 mph or greater.

What is the "eye" and "eyewall"?

The eye is a feature which is unique to strong tropical cyclones like hurricanes (or typhoons). Warm, moist air spiraling into the center of a hurricane reaches a point where it no longer tracks into the center. Instead, it rises up into the atmosphere as high as 10 miles, forming the eyewall. The eyewall is a circular ring of intense squalls surrounding the center of a hurricane and contains a hurricane’s strongest winds. This ring of intense squalls can be as small as one mile or as large as 100 miles in diameter. Inside the eye, close to the center, the winds are relatively calm, often less than 25 mph.

What is a popular hurricane myth?

A particularly dangerous “myth” is the misconception that a hurricane’s storm surge is a direct function of its Saffir-Simpson category (i.e. a Category 3 storm). Many hurricane response plans are based on a hurricane’s Saffir-Simpson ranking. For example, a coastal business may have a plan that only requires evacuation for a Category 3 hurricane or greater. There are a number of variables that contribute to storm surge, and its Saffir-Simpson ranking is only a slight factor. Much more significant is the size of the hurricane’s wind field—a large Category 2 hurricane will produce a greater storm surge than a small Category 4 or 5 hurricane. Every hurricane is different, so never rely solely on a hurricane’s Saffir-Simpson ranking to estimate storm surge. In fact, StormGeo has developed the Hurricane Severity Index, which looks at wind speeds and the size of the wind field to classify hurricanes based on their potential for damage. Read more about the Hurricane Severity Index. 

Tropical Storm Forecast for 2022

For a full look into our predictions for the 2022 Atlantic Hurricane season, read our forecast here. In the meantime, here are a few key takeaways:

The 2021 Atlantic Hurricane Season was the third most-active season on record with 21 named storms, 7 of which were hurricanes, including 4 major (category 3 or higher) hurricanes. Looking ahead to the upcoming season, there are a number of signals that StormGeo's Hurricane and Long-Range Forecasters evaluate to determine the seasonal outlook, including:

• the formation of El Niño or La Niña,
• Atlantic oceanic heat content,
• the presence of low-level wind shear in the main development region of the Atlantic, and
• analog seasons.