section_path: Geography/Climate
section_name: Climate
paragraph_text: Climate
  
  Most of Egypt's rain falls in the winter months. South of Cairo, rainfall averages only around 2 to 5 mm (0.1 to 0.2 in) per year and at intervals of many years. On a very thin strip of the northern coast the rainfall can be as high as 410 mm (16.1 in), mostly between October and March. Snow falls on Sinai's mountains and some of the north coastal cities such as Damietta, Baltim and Sidi Barrani, and rarely in Alexandria. A very small amount of snow fell on Cairo on 13 December 2013, the first time in many decades. Frost is also known in mid-Sinai and mid-Egypt.
  
  Egypt has an unusually hot, sunny and dry climate. Average high temperatures are high in the north but very to extremely high in the rest of the country during summer. The cooler Mediterranean winds consistently blow over the northern sea coast, which helps to get more moderated temperatures, especially at the height of the summertime. The Khamaseen is a hot, dry wind that originates from the vast deserts in the south and blows in the spring or in the early summer. It brings scorching sand and dust particles, and usually brings daytime temperatures over 40 °C (104 °F) and sometimes over 50 °C (122 °F) in the interior, while the relative humidity can drop to 5% or even less.
  
  Prior to the construction of the Aswan Dam, the Nile flooded annually, replenishing Egypt's soil. This gave Egypt a consistent harvest throughout the years.
  
  The potential rise in sea levels due to global warming could threaten Egypt's densely populated coastal strip and have grave consequences for the country's economy, agriculture and industry. Combined with growing demographic pressures, a significant rise in sea levels could turn millions of Egyptians into environmental refugees by the end of the 21st century, according to some climate experts.