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Saline Intrusion due to the Accelerative Sea Level in the Red River System in Vietnam

机译:越南红河系统中加速的海平面导致盐渍入侵

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Global climate change accelerates the sea level. Numerous investigations confirm that the indirect effect may be more significant than the direct effects by the rising sea level in this century; that is, it increases salinity of rivers and estuaries. The implications of sea level rise for increasing of salinity were examined for four estuary branches in the Red River System in North Vietnam using Savenije's salt-intrusion model, based on salinity data acquired in the dry season of 2006. By correlative analysis of river discharge, tidal range, and geometric characteristics, the changes of salt intrusion length and longitudinal salinity profile were estimated for three different sea levels: M.S.L.+30 cm, +75 cm, and +100 cm. It was found from the calculations that the saltwater intrusion extends 31-50% when the sea level is increased 100 cm by the year 2100. Most of the estuary branches are highly vulnerable to the sea level rise.
机译:全球气候变化加速了海平面。许多研究证实,在本世纪中,间接影响可能比海平面上升带来的直接影响更为显着。也就是说,它增加了河流和河口的盐度。根据Savenije的盐分入侵模型,基于2006年干旱季节获得的盐度数据,研究了越南北部红河系统中四个河口分支的海平面上升对盐分增加的影响。估计了三个不同海平面的潮汐范围,几何特征,盐侵入长度和纵向盐度剖面的变化:MSL + 30 cm,+ 75 cm和+100 cm。通过计算发现,到2100年,当海平面上升100 cm时,盐水的入侵将扩展31-50%。大多数河口分支极易受海平面上升的影响。

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