Table of Contents
Typhoons are powerful tropical storms that are influenced by various physical features of the Earth’s surface and atmosphere. Understanding these features helps in predicting their behavior and potential impact.
Sea Surface Temperatures
Warm sea surface temperatures are a primary factor in the development and intensification of typhoons. Temperatures above 26.5°C provide the energy necessary for storm formation and strengthening.
Coriolis Effect
The Coriolis effect, caused by Earth’s rotation, influences the rotation and path of typhoons. It is stronger near the equator and helps in the initial spinning of the storm.
Topography and Land Interaction
Mountain ranges and landmasses can disrupt typhoon movement and weaken storms through friction and reduced moisture supply. Land interaction often leads to a decrease in storm intensity.
Wind Shear
Vertical wind shear, the change in wind speed or direction with altitude, can inhibit or enhance typhoon development. Low wind shear favors storm intensification, while high shear can weaken or displace the storm.