The five-year depressions are a decrease in the atmospheric pressure values and are formed in the regions of the desert of Algeria, east of the Moroccan Atlas Mountains. This system of low air pressure moves quickly through the deserts of Libya and Egypt directly towards the eastern basin of the Mediterranean and the Levant region.
It was called the Khamasiyya, because its duration is fifty in the period from the vernal equinox to the 21st of March of each year until 10 May of each year .
The Khamaseen winds accompany the Khamasine depression, which is a southeastern seasonal wind loaded with dust and dust, and its source is as we mentioned earlier, the Sahara, which occupies the largest part of North Africa, and its impact reaches the Levant countries, Egypt, and the Arab Gulf states, in addition to Iraq and Yemen.
This wind is characterized by being hot and dry winds and loaded with dust and dust.
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