Destructive Factors

Tide

In Abaco the high tide ranges from 3.5 - 4 feet and it occurs once a day.

The mean tide would be around 2 feet.

Storm Surge

Storm surge is simply water that is pushed toward the shore by the force of the winds swirling around the storm. The height of the surge is dependent on the characteristics of the storm, and the make-up of the shoreline and sea floor.

Hurricane driven surge

 

Surge Factors from Storm Characteristics

            -The more intense the storm (i.e. higher wind speeds), the higher the wave heights and storm surge.

            -The faster the storm moves, the quicker the surge piles up and the harder it strikes.

            -Generally, the more perpendicular the storm hits, the higher the surge will be. Also, bays and inlets increase the storm surge height.

Surge Factors from Shoreline and Sea Floor Characteristics

    -Bays, headlands and offshore islands can funnel and amplify the storm surge.

            -The surge builds up more strongly if the slope of the sea bed at the coast is shallow. If the sea bed slopes steeply, or if fringing reefs are present, then the surge will be less.

        

 

The Saffir-Simpson Scale for Hurricane Classification gives a general idea of storm surge based on the wind speeds and category of the hurricane:

Saffir-Simpson Scale for Hurricane Classification
 
Strength Wind Speed
(kt)
Wind Speed
(mph)
Pressure
(millibars)
Pressure
(inches Hg)
Storm Surge
(ft.)

Category 1

65-82 kt

74-95 mph

>980 mb

>28.94 in.
 

4-5 ft.
 

Category 2

83-95 kt

96-110 mph

965-979 mb

28.50-28.91 in.
 

6-8 ft.
 

Category 3

96-113 kt

111-130 mph

945-964 mb

27.91-28.47 in.
 

9-12 ft.
 

Category 4

114-135 kt

131-155 mph

920-944 mb

27.17-27.88 in.
 

13-18 ft.
 

Category 5

>135 kt

>155 mph

<919 mb

<27.16 in.
 

>18 ft.
 

Tropical Cyclone Classification

Tropical Depression

20-34 kt or 23-39 mph

Tropical Storm

35-64 kt or 40-73 mph

Hurricane

65+ kt or 74+ mph

 

Wave Heights

Wave heights during a hurricane can be very large as shown in the following diagrams. The heights and breaking points depend on the shoreline characteristics, but are devastating non e the less.

 

 

            Wind graph