Arab Weather - The latest outputs of the numerical models operated internally in Arab weather indicate a decline in the subtropical air altitude and an expected retreat and decline of the atmospheric thermal depression, where it is expected that there will be a further decrease in temperatures during the weekend, and the following are the details:
In the details, it is expected that moderate-temperature air currents will increase in the country, so that mild autumn weather will prevail in coastal areas, Lower Egypt and Greater Cairo, all the way to northern Upper Egypt, and hot in southern Upper Egypt. Winds will be northwesterly moderate speed, active in the afternoon, and be dusty. And dust in some areas, especially the coast of the Red Sea and the southern regions, with the appearance of some low clouds in the northern regions in the morning and noon.
During the night hours, pleasant weather prevails throughout the northern regions, tending to be cold in the late night hours in some areas, while it is warm in the southern regions, and humidity levels rise and water mist is formed in parts of Sinai and the canal cities, and the winds are north to northeast. Moderate speed in general.
The opportunity is set for sporadic showers of rain on parts of the northern coast, which may extend to a limited extent to include the northern delta, from the night hours on Friday until the daylight hours on Saturday.
These autumn weathers come as a result of the distribution of air systems that worked to rush moderate air masses towards the eastern Mediterranean, as a result of the displacement of the jet stream south over the atmosphere of the northern Arabian Peninsula and the building of the upper air altitude eastward from the Levant, where it was located in the upper air layers of Egypt as an extension of air depressions that By mitigating the heat through the leakage of heat rays from the surface of the Earth to the top, and this led to a softening of the atmosphere, and on the other hand, the surface was free of deep low atmospheric pressure centers, which contribute to the circulation of winds and bring hot masses.
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