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When this wind blows over Egypt, it causes high temperatures to soar temporarily at dangerous levels, usually over 49–50 °C (120–122 °F), the relative humidity levels to drop under 5%. The khamasīn causes sudden, early heat waves and the absolute highest temperature records in Egypt.
At the site of Sidi Ali in the Middle Atlas, δ 18 O values indicate not a dry spell but a centennial-scale period of cooler and more humid climate. [40] In c. 2150 BC, Egypt was hit by a series of exceptionally low Nile floods that may have influenced the collapse of the centralised government of the Old Kingdom after a famine. [41]
The climate of the Qattara Depression is highly arid with annual precipitation between 25 and 50 mm (0.98 and 1.97 in) on the northern rim to less than 25 mm (0.98 in) in the south of the depression. The average daily temperature varies between 36.2 to 6.2 °C (97.2 to 43.2 °F) during summer and winter months.
Climate change occurs when changes of Earth's climate system result in new weather patterns that remain for an extended period of time. This duration of time can be as brief as a few decades to as long as millions of years. The climate system receives nearly all of its energy from the sun. The climate system also gives off energy to outer space.
Egypt's location. The geography of Egypt relates to two regions: North Africa and West. Egypt has coastlines on the Mediterranean Sea, the River Nile, and the Red Sea.Egypt borders Libya to the west, Palestine and Israel to the east and Sudan to the south (with a current dispute over the halaib triangle).
Egypt's fresh water is mainly derived from underground water. Underground water results in 95% of Egyptian's desert land. Egypt is also dependent on rainwater but it is a scarce and limiting source for agricultural development. In addition, Egypt refuses agricultural drainage water in correlation with Nile water for irrigation. [2]
The Köppen climate classification divides climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are A (tropical), B (arid), C (temperate), D (continental), and E (polar).
The end of the Neolithic Subpluvial era and return of extremely hot and dry conditions in the Sahara Desert, hastened by the 5.9 kiloyear event and the Piora Oscillation. 3500 BC 3200 BC Gerzeh/Naqada II culture in Egypt 3200 BC 3000 BC Naqada III and Protodynastic Period of Egypt: 3100 BC 2686 BC Early Dynastic Period of Egypt.
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