|
Causes of Hurricane Damage |
|||
|
Cause |
Component | Comments | |
|
Flooding |
"Storm Surge" | Elevation
of sea level caused by low surface barometric pressure |
"Sea level" rises in response to a pressure drop by about ~1 cm/mb |
| Ekman transport | Is
greatest when winds are parallel to the shoreline with land to the right of
the direction towards which the wind is blowing. |
||
| Waves (can approach 50 feet in height) | Are worst when the wind direction is directly onshore. | ||
| High tides | When the storm surge occurs at high tide its destructive effects are worsened. | ||
| Rain-induced | Some
hurricanes have dumped more than 20 inches of rain. This is the main cause of inland damage associated with hurricane remnants. |
||
| Landslides | Rain-induced | Not a major
problem in the USA because hurricane-vulnerable coastal regions have little vertical relief. Sometimes a major problem in mountainous coastal regions such as occur in much of Central America and some islands of the West Indies. |
|
| Wind | Wind from hurricane circulation | Can exceed 155 mph in category 5 storms. | |
| Hurricane-spawned tornadoes | Occur in about one quarter of all hurricanes. | ||
| Spin-up vortices | Small
eddies 30 to 100 meters in diameter which may rotate at speeds as high as 70 knots (80 mph). Much like small tornados, these occur in or near the eye wall and persist for about 10 seconds. Such a vortex, in a strong hurricane, can produce a brief episode of total wind speeds exceeding 200 mph. |
||