Galveston.com  General Hurricane Facts You Need to Know

FACTS TO KNOW

General Hurricane Facts You Need to Know

For up-to-the-minute weather information, visit the Galveston.com Weather Center, from weatherman Stan Blazyk, our @GalvWeather account on Twitter, and our two WeatherUnderground Weather Stations - on The Strand and Seawall Boulevard!

Hurricanes, Cyclones, Typhoons - by whatever name, tropical systems are some of the most deadly storms known to man. However, as we've learned more about the nature of these storms, we've improved forecasting accuracy and increased warning time to those in the path of the storm.

Hurricane Season in the Atlantic runs from June 1 to November 30.  The activity ramps up in August and peaks once in early September then again in October. Persons travelling to areas near the Atlantic basin should exercise caution during Hurricane Season.

The Anatomy of a Tropical Storm

Cross Section of a Hurricane

  1. Outflow: The high level clouds moving clockwise out away from the hurricane at heights of over 35,000 feet. These clouds are indicative of air spreading out over the top of the storm, which is essential to its development.
  2. Feeder Bands: These are squally bands of showers characterized by strong gusty winds and heavy rains. These bands become more pronounced as the storm intensifies, and are fed by the warm ocean.
  3. The Eyewall: A band of clouds, strong winds and heavy rains surrounding the eye of the storm. At the eyewall, there is rapid movement of air toward the center and upward into the cloud.
  4. The Eye: What goes up must come down, so with the violent rising air converging toward the storm center at the eye, sinking air develops within. This air dries out, creating the clear, calm eye. Winds are very light here since the focus of convergence and hence strong winds are in the eyewall.

Storm Surge / Storm Tide

STORM SURGE is an abnormal rise of water generated by a storm’s winds. Storm surge can reach heights well over 20 feet and can span hundreds of miles of coastline. In the northern hemisphere, the highest surge values typically occur in the right front quadrant of a hurricane coincident with onshore ow; in the southern hemisphere, the left front quadrant. More intense and larger hurricanes produce higher surge. In addition, shallower offshore waters contribute to higher storm surge inundation. Storm surge is by far the greatest threat to life and property along the immediate coast. 

STORM TIDE is the water level rise during a storm due to the combination of storm surge and the astronomical tide. For example, if a hurricane moves ashore at a high tide of 2 feet, a 15 foot surge would be added to the high tide, creating a storm tide of 17 feet. The combination of high winds and storm tide topped with battering waves can be deadly and cause tremendous property damage along an area of coastline hundreds of miles wide.

The destructive power of storm surge and large battering waves can result in loss of life, buildings destroyed, beach and dune erosion and road and bridge damage along the coast. Storm surge can travel several miles inland. In estuaries and bayous, salt water intrusion endangers public health and the environment. 

Historical Storm Tide Events

  • 1900: Galveston, TX, hurricane, resulted in more than 8,000 deaths, most by storm tide. „
  • 1969: Hurricane Camille produced a 24-foot storm tide in Mississippi. „
  • 1989: Hurricane Hugo generated a 20-foot storm tide in South Carolina. „
  • 1992: Hurricane Iniki produced a 6-foot storm tide on the island of Kauai in Hawaii. „
  • 2005: Hurricane Katrina generated a 27-foot storm tide in Mississippi. „
  • 2008: Hurricane Ike produced a 20-foot storm tide in Texas.

Tropical Storm Development

Step 1
Tropical Wave: "bump" or disruption of normal tropical easterly flow. Associated turning of wind causes low-level convergence of air; which helps with falling pressure and enhanced showers.

Step 2
This can evolve into a Tropical Depression, which is a closed circulation of air in the low levels. This in turn increases convergence and pressure falls, and wind speeds increase in a Catch-22 effect (i.e. the stronger the wind blows the greater the convergence, the quicker the pressure falls... so the stronger the wind, etc.).

Step 3
Once sustained winds reach 39 mph in the closed circulation a Tropical Storm is named. Usually there are at least 2 closed isobars of 4 mb increments around the center. If atmospheric conditions remain correct the system will evolve into a...

Step 4
Hurricane. There is usually a difference in pressure of at least 0.60 inches of mercury between the center and surrounding pressure field, with the greatest change near the center (eyewall). It is this great difference in pressure, which sometimes can be as great as 2.95 inches of mercury, that causes the wind to be so strong.

Step 5
A mature hurricane is a well-oiled meteorological machine, but disruption of the processes that drive the storm (i.e. interaction with land or colder air feeding in) will begin to destroy the storm, and the disintegration of a hurricane can often be quick and dramatic.

Hurricane Categories

Hurricanes are evaluated in a number of ways. Storms are assigned a category based on winds, storm surge and barometric pressure, using the Saffir-Simpson scale.

Category 1 storms have winds of 74-95 miles per hour, making them the weakest of hurricanes. Even these storms can generate a storm surge of 4 or 5 feet above normal high tide.

Category 2 storms have winds of up to 110 miles per hour, and can push a storm surge of 6 to 8 feet.

Category 3 storm winds can reach 130 miles per hour. This is the cutoff for "major" hurricanes, with commensurate storm surge potential of 9 to 12 feet.

Category 4 winds can be as high as 155 miles per hour, and such a storm brings a 13 to 18 foot storm surge.

Category 5 storms, with winds greater than 155 miles per hour, are very rare. These monsters can have storm surges of over 20 feet.