The tropical season in the Arabian Sea is approaching. Will the first tropical cyclone activity be recorded soon?

Arab Weather - The latest climate data indicates that the surface temperatures of the Arabian Sea and the northern Indian Ocean, including the Bay of Bengal, have risen to around 30 degrees Celsius. This rise is significant and important from a meteorological perspective, as these temperatures are within the ranges favorable for the development of tropical conditions, such as tropical depressions, storms, or even hurricanes, if other supporting weather factors are present. Warm waters are a key catalyst for feeding and condensing cumulus clouds, which enhances the chances of tropical weather systems emerging in these marine areas in the coming period.

Scientifically: Weather conditions are hindering the development of the tropical system into the first storm in the Arabian Sea this year.

Scientifically speaking, meteorologists at the Arab Weather Center noted that although high surface temperatures are one of the reasons for the development of tropical systems, they also noted the presence of obstacles preventing the development of tropical conditions in the Arabian Sea at the present time. These obstacles can be summarized in the following points:

Upper shear winds:

The computer outputs reveal the presence of strong upper wind shear over the Arabian Sea and surrounding areas. In the case of tropical systems such as cyclones or tropical depressions, strong wind shear weakens the atmospheric system or even prevents it from developing (just as it does in the Arabian Sea). This effect occurs because wind shear separates and disperses the structure of the atmospheric system, shearing and separating the upper and lower layers of the system, weakening the integration of clouds and convection necessary for cyclone or depression development. In the Arabian Sea, when there is strong wind shear, it hinders the tropical system from receiving the moisture and energy it needs to deepen. Wind shear is a change in wind speed or direction with height in the atmosphere.

The presence of an upper atmosphere:

At the upper level, the absence of other weather systems is a necessary condition for tropical systems to develop. However, in the case of the Arabian Sea, a strong high pressure system, a layer of compressed air at the upper levels of the atmosphere, is present in the upper atmosphere. Meteorologists say that the presence of this high prevents the tropical system from penetrating horizontally into the upper atmosphere because it imposes downward pressure and enhances sinking currents. This impedes the upward rise of warm, moist air from the surface, which is essential for the system to strengthen and develop.

The first tropical cyclone season of the year is approaching in the Arabian Sea and northern Indian Ocean.

The first season of tropical activity in the Arabian Sea is known as the "pre-monsoon," which precedes the monsoon. This season typically occurs during May and June. During this season, sea surface temperatures are warm enough and wind shear is relatively weak, providing a favorable environment for the development of tropical conditions. This period is considered one of the most prominent periods that may witness the formation of tropical depressions or cyclones in the Arabian Sea, before the southwest monsoon begins to affect the region during the summer.

And God knows best.