Storm Surge

A storm surge is an abnormal rise in sea level driven by atmospheric pressure changes and strong winds during severe storms, particularly hurricanes and cyclones.

Storm Surge

A storm surge represents one of the most dangerous aspects of coastal storms and tropical cyclones, characterized by an unusual rise in sea level that can devastate coastal areas. This phenomenon occurs when powerful storms push water toward the shore through a combination of wind forces and atmospheric pressure changes.

Formation Mechanics

The development of a storm surge involves several key mechanisms:

  1. Wind-Driven Water Movement
  • Strong wind patterns push surface water toward the coastline
  • Coriolis effect influences the direction of water movement
  • Sustained winds create a cumulative piling effect
  1. Pressure Effects
  • Low atmospheric pressure at the storm's center causes water levels to rise
  • Every 1 millibar drop in pressure can raise water levels by approximately 1 centimeter

Contributing Factors

Several environmental conditions can amplify storm surge severity:

Impact and Risks

Storm surges pose significant threats to:

Physical Infrastructure

Environmental Effects

Prediction and Monitoring

Modern storm surge prediction relies on:

Mitigation Strategies

Communities employ various approaches to reduce storm surge impacts:

  1. Structural Measures
  1. Non-Structural Measures

Historical Examples

Notable storm surges have caused catastrophic damage throughout history, including:

Climate Change Implications

Rising sea levels and increasing storm intensity due to climate change may lead to:

  • More frequent extreme surge events
  • Higher baseline water levels
  • Greater coastal vulnerability
  • Enhanced need for coastal adaptation strategies