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Physical Limnology of Bardawil Lagoon, Egypt

机译:埃及巴尔达维尔泻湖的物理湖沼学

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Bardawil lagoon is suffered from many problems, which might lead to environment degradation, shortage in fish catch and substantial changes in its ecosystem. The present study was carried out to evaluate Bardawil Lagoon from a physical limnology, through investigation of; climate bathymetry and salinity. Bardawil is a costal lagoon located along the Mediterranean shore of the Sinai region (31°09N, 33°08E), Egypt. Over Bardawil Lake, there are two climate periods, rainy season (November to April) and dry season (May to October). The lagoon extends for about 76.37 km length and has a maximal width of 16.65 km, with area of approximately 518.99 km . Bardawil Lagoon is extremely shallow; the average water depth is of 1.2 m. The whole 2 water supply of the lagoon comes from the Mediterranean Sea which flows constantly through two openings. The spatial variability observed in the water salinity of the lagoon. The highest salinities reached along the southern shore. The temporal variations of water salinity in the lagoon are in equilibrium between the evaporation and the sea water exchange. There are difficult to determine the annual trend in the water salinity of the lagoon.
机译:巴尔达维尔泻湖遭受许多问题的困扰,这可能导致环境退化,鱼品短缺和生态系统的重大变化。本研究旨在通过物理研究从物理学上评估Bardawil泻湖;气候测深和盐度。巴尔达维尔(Bardawil)是位于埃及西奈地区(31°09N,33°08E)地中海沿岸的沿海泻湖。 在巴尔达维尔湖上,有两个气候时期,雨季(11月至4月)和旱季(5月至10月)。泻湖的长度约为76.37 km,最大宽度为16.65 km,面积约为518.99 km。巴尔达维尔泻湖非常浅。平均水深为1.2 m。泻湖的全部2供水都来自地中海,该地中海不断流经两个开口。泻湖水盐度中观察到的空间变异性。最高的盐度达到了南部海岸。泻湖中水盐度的时间变化在蒸发和海水交换之间处于平衡状态。很难确定泻湖水盐度的年度趋势。

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