Arab weather - Northern Algeria is gradually affected by a state of atmospheric instability during Wednesday, as the weather is relatively hot in the northern regions and very hot in the rest of the regions, and gradually multiplies with the passage of daylight hours, amounts of clouds at different altitudes, and the opportunity for thunder showers is created. From rain, God willing, in random and scattered areas in the north of the country, especially the interior areas.
As the night falls, the northern regions are more affected by the state of atmospheric instability, and it is expected that it will be strong in some areas. The weather is generally relatively cold with the appearance of clouds at different altitudes, and thunder showers of rain are expected, God willing, in random areas in the north of the country. and reefs, and these thunder showers are accompanied by strong gusts of wind.
Weather disturbances will continue in the northern regions of Algeria on Thursday, so that the opportunity remains prepared for thunder showers of rain, God willing, in random areas of the north of the country, as well as extending to the northern parts of the desert, and some of these showers are heavy in some neighborhoods and narrow geographical areas, accompanied by It is hail that causes the flow of valleys and reefs.
The chances of rain extend during the day Thursday hours to parts of Tunisia, especially the western highlands and parts of the central region, with its concentration in the governorates of (Kasserine, Gafsa, Sidi Bouzid). The rain is heavy in some neighborhoods and narrow geographical areas, accompanied by hail, which causes the flow of valleys and reefs, and these thunder showers are accompanied by strong gusts of wind. It is expected that Algeria and Tunisia will be affected over the weekend by the state of atmospheric instability resulting from the convergence of an extension of a shallow air depression in the Algerian desert and a cold air mass in the upper layers of the atmosphere, in addition to that this convergence coincides with the flow of moisture in the different layers of the atmosphere.
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