Why is the Wasm season characterized by frequent thunderstorms?

As soon as the Wasm season begins in the Kingdom of Saudi Arabia, unstable weather conditions begin to affect the region in an escalating manner. This is accompanied by a noticeable increase in thunderstorm activity compared to other times of the year. This activity is due to a number of atmospheric factors that create an ideal environment for the formation of cumulus clouds, lightning, and thunderbolts. These factors include:

Thermal differences between air masses

During the Wasm season, Saudi Arabia experiences significant temperature differences between atmospheric layers, as cold air masses advance from the north and meet warm, humid air masses coming from the south. This convergence creates atmospheric instability, leading to the formation of high-altitude cumulonimbus clouds accompanied by lightning, thunder, and lightning.

Red Sea Low Activity:

The Red Sea low pressure contributes to pumping more moisture into the lower layers of the atmosphere, which enhances the upward movement of warm, humid air and increases the density of thunderstorms. This interaction between low humidity and cold air masses makes storms more severe and frequent during the Wasm season.

In short, the Wasm season witnesses intense thunderstorm activity in Saudi Arabia due to the convergence of cold, northern air masses with warm, humid, southern air masses and the activity of the Red Sea low pressure system. This makes it a period of intense rainfall and lightning in the western and southwestern regions of the Kingdom.