Storm Surge vs. Storm Tide

How the SLOSH Model Works

Given a specific geographic region (a SLOSH Basin), the model takes a hypothetical or historical hurricane track and calculates the resulting storm surge.

Model Inputs

Model Accuracy and Limitations

Storm Surge Generalizations

When observing storm surge animations, several meteorological generalizations apply:

  1. More intense storms cause higher surges.
  2. The highest surges usually occur to the right of the storm track.
  3. Fast-moving storms cause high surges along the open coast and lower surges in sheltered bays and estuaries.
  4. Slow-moving storms usually result in greater flooding inside bays and estuaries, with smaller values along the open coast.
  5. Larger storms (greater radius of maximum winds) affect longer stretches of the coastline.
  6. A shallow coastal slope will allow a greater storm surge with small waves, while areas with steep coastal slopes experience less surge but large breaking waves.

Interpreting Rex-files and Wind Data

A Rex-file contains SLOSH-generated water level heights at each grid cell and hurricane wind parameters for specific time intervals. When animating a Rex-file in the SDP, wind speeds and directions are displayed using standard meteorological conventions:

Wind Barb Symbology

Wind Scale Colors