Maghreb | Active turbulence and several areas concerned with rain in the coming days
Arab weather - The outputs of computer numerical models still indicate that several regions of the Maghreb are affected by a state of instability resulting from the deepening of a seasonal desert air depression over the Algerian desert, which works to pump moisture from the African tropics, in conjunction with the approach of a cold air mass in The upper layers of the atmosphere, which leads to a thermal imbalance for the multiplication of cumulonimbus thunderclouds in many areas, God willing.
Tuesday and Wednesday
Active turbulence affecting Algeria and Morocco
In the details, it is expected, God willing, that rainy thunder clouds will form throughout the northern parts of Morocco, in addition to large parts of northern Algeria and random parts of the Algerian desert, on Tuesday and Wednesday, March 29 and 30, 2022, and it is expected that heavy rain will fall at intervals, accompanied by lightning and thunder. And hail showers may fall, with a relatively high chance of torrential rain, especially on the mountain slopes. At the same time, the southern winds are active in parts of Algeria, especially the western ones, and are working to form dust waves in many areas, God willing.
Thursday and Friday
The unrest has receded from Morocco, and the rains have focused on Tunisia and northern Algeria
In the direction of Thursday, the desert air depression moves north and is centered near the Tunisian lands, and the winds turn to northwest, so that the chances of rain improve in northern Tunisia, God willing, with the chances of rain still appearing in the northern parts of Algeria, especially the coastal ones, and these rains are heavy at times. And accompanied by lightning and thunder at times, and showers of hail in some areas.
During the impact of weather disturbances, Arabia Weather warns of:
- Intensity of thunderstorms.
- The danger of torrential rains.
- Intensity of downward winds associated with thunderstorms.
- Danger of reduced horizontal visibility due to dust waves caused by downward winds.
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