Hurricane and Extreme
Storm Impact Studies
Hurricanes, El-Niņo, & Northeasters
- An Introduction
| At present, USGS investigates three types of severe coastal storm impacts: hurricane impacts on the southeast U.S., extra-tropical storm impacts on the U.S. west coast during El-Niņo winters, and 'northeaster' impacts on the U.S. east coast. Hurricanes are tropical
storms that have a sustained wind speed greater than 75MPH. In the northern
hemisphere, these low pressure systems rotate counterclockwise. As a
hurricane approaches the coast, the wind speed on the right side of
the storm is added to the forward speed of the storm. Hence, the greatest
impacts from storm surge, wave battering and wind speed tend to occur
to the right of the eye at landfall. Storm surge is an increase in sea
level along the coast caused primarily by strong onshore winds and low
barometric pressure. The strongest hurricanes are Category 5, having
sustained wind speeds in excess of 155MPH and storm surge in excess
of 6 m (20 ft). In recorded history, only two Category 5 hurricanes
have made landfall in the United States.
During severe El-Niņo,
the jet stream over the Pacific Ocean tends to be more southerly than
normal, guiding winter extra-tropical storms into California and bringing
extensive rainfall and large waves to the California coast. During the
severe El-Niņo's of 1982-83 and 1997-98 extensive coastal erosion and
damage occurred along the west coast. Under El-Niņo conditions of equatorial
warming in the Pacific, hurricanes are less frequent in the north Atlantic.
The reoccurrence of La-Niņa, equatorial cooling in the Pacific, coincides
with active hurricane seasons for the southeast United States.
Northeasters, or winter extra-tropical storms impacting the east coast of the United States, can cause considerable coastal change and damage. For example, one of the most destructive storms to ever impact the mid-Atlantic states was the Ash Wednesday storm of 1962. Extensive coastal change occurred over 1,000 km of coast. Northeasters owe their destructive power to their long duration. Winds are typically below hurricane force, but can persist for several days to a week generating large waves and enhanced storm surge. In comparison, hurricanes are more severe in terms of wind speed and storm surge but the shoreline impacts tend to be more localized, confined to order 100 km of coast. Hurricanes also tend to be more short-lived moving across coastal areas in hours rather than days. |