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The cold prevailing northwesterly wind from Greece continuously blows over the northern coast without the interposition of an eventual mountain range and thus, greatly moderates temperatures throughout the year. Because of the effect, average low temperatures vary from 15 °C (59 °F) in wintertime to 27–35 °C (80.6–95.0 °F) in summertime ...
In general, Egypt is a very dry country. The Western Desert receives only occasional rainfall, the winters being mild and the summers very hot. The Eastern Desert receives some precipitation in the south in the form of orographic rainfall from winds that have crossed the Red Sea; this may cause torrential flows in the wadis. The winters here ...
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]
Egypt is located on the northeast of the continent of Africa. The population was 102.3 million in 2020 and is projected to grow to 159.9 million by 2050. [2] Egypt is one of the countries most affected by the extreme weather conditions caused by climate change. [3]
Wind and moist air are drawn by the prevailing winds towards the top of the mountains, condensing and precipitating before it crosses the top. In an effect opposite that of orographic lift, the air, without much moisture left, advances behind the mountains, creating a drier side called the "rain shadow". [citation needed]
Gabal Elba (Arabic: جَبَل علْبَة Gabal ʿElba, Egyptian Arabic pronunciation: [ˈɡæbæl ˈʕelbæ], "Box Mountain"), or Elba Mountain refers to the mountain itself as well as the mountainous area in the Halaib Triangle of Northeast Africa. It is claimed by both Egypt and Sudan, but is under Egyptian control.
An orographic map of Eastern Siberia from 1875 by Peter Kropotkin. Orography is the study of the topographic relief of mountains, [1] and can more broadly include hills, and any part of a region's elevated terrain. [2] Orography (also known as oreography, orology, or oreology) falls within the broader discipline of geomorphology. [3]
Thundersnow is possible within a cyclone's comma head and within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation. On the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating.