Once built up, the dunes are affected by the summer NW sea breeze, a gentler wind with high frequency that becomes the dominant wind in north western Sinai. The coastal dunes in Israel are oriented according to the SW and W dominant winter storm winds (Figure 27a). All the rain falls between September and May, while most of it is fallen between December and February. The average annual amount of rainfall in the western Sinai coast is 80mm, increasing to 200mm in Rafah, at the boundary between Egypt and the Gaza Strip, and up to 600mm in the northern coastal plain of Israel. This coastal dune strip stretches between arid and sub-humid climates characterized by hot, dry summer, and mild, and relatively wet winters. They comprise of a young dune field whose age, estimated to be around 1000 years, according to archaeological sites of Byzantine age (5th - 6th century AD) underlie the dunes (Tsoar 1990). The coastal sand dunes include those of Israel, Gaza Strip (Figure 27) and extend into Sinai. The Israeli coastline (190km, from Gaza Strip to Lebanon) forms part of the south eastern Mediterranean. Author: Haim Tsoar new text 2008, site list Dr. These represent chapters from updated individual country reports included in the revised, 2nd Edition of the 'Sand Dune Inventory of Europe' prepared for the International Sand Dune Conference “Changing Perspectives in Coastal Dune Management”, held from the 31st March - 3rd April 2008, in Liverpool, UK (Doody ed. It attempted to provide a description of the sand dune vegetation, sites and conservation issues throughout Europe including Scandinavia, the Atlantic coast and in the Mediterranean.Īn overview article on European sand dunes provides links to the other European country reports. The original inventory was presented to the European Coastal Conservation Conference, held in the Netherlands in November 1991. ![]() The 1991 inventory was prepared under the umbrella of the European Union for Dune Conservation. This article on the sand dunes of Israel, is a new country report and represents an addition to the 'Sand Dune Inventory of Europe' (Doody ed.
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