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The Sudd (' or ') is a vast swamp in South Sudan, formed by the White Nile's ''Baḥr al-Jabal'' section. The Arabic word ' is derived from ' (), meaning "barrier"〔Gaudet, J.J., and A. Falconer, 1983. Remote sensing for tropical freshwater bodies. The problem of floating islands on Lake Naivasha. Regional Remote Sensing Facility, Nairobi, Kenya. 4p.〕 or "obstruction".〔The ''New Oxford American Dictionary'' (''NOAD''), 3rd edition.〕 The term "the sudd" has come to refer to any large solid floating vegetation island or mat. The area which the swamp covers is one of the world's largest wetlands and the largest freshwater wetland in the Nile basin. For many years the swamp, and especially its thicket of vegetation, proved an impenetrable barrier to navigation along the Nile. For this reason, the search for the source of the Nile was particularly difficult; it eventually involved overland expeditions from the central African coast, so as to avoid having to travel through the Sudd. ==Location== The Sudd stretches from Mongalla to just outside the Sobat confluence with the White Nile just upstream of Malakal as well as westwards along the Bahr el Ghazal. The shallow and flat inland delta lies between 5.5 and 9.5 degrees latitude North and covers an area of south to north and east to west between Mongalla in the south and Malakal in the north. Its size is highly variable, averaging over . During the wet season it may extend to over , depending on the inflowing waters, with the discharge from Lake Victoria being the main control factor of flood levels and area inundation. Since the Sudd area consists of various meandering channels, lagoons, reed and papyrus fields and loses half of its inflowing water through evapotranspiration in the permanent and seasonal floodplains, the complex hydrology has many primary and secondary effects. A major feature of the area, even if not completed and not functional, is the Jonglei Canal, planned to bypass waters from the Sudd to avoid evaporation losses and increase the amount of water discharged at the outlet of the Sudd. From 1961 to 1963, a great increase in the inundated area occurred when the level of Lake Victoria rose and the outflow increased. The total area of the Sudd is related to the amount of water reaching Bor from Albert Nile and from torrents or seasonal watercourses that can add substantial amounts to the flow in the upstream end of the Sudd. During the 1960s increase in Lake Victoria discharge, where flows at Mongalla roughly doubled, the flows at Malakal at the northern end of the swamps increased by 1.5 times the previous average flow. As a consequence of these high flows, the areas of permanent swamp and seasonal floodplains have, taken together, increased to 2.5 times their former size. The swamps have increased the most, and the seasonal floodplain is 1.5 times its previous size. From the southern inflow of the Bahr al Jabal ("Sea of the Mountain") at Mongalla, the defined riverbed successively widens into a floodplain, where the waters flow in meandering river stretches and various channels and lagoons throughout the dry season. With rising water levels it expands over the semi-flooded grasslands during the flood season. Slightly downstream of Bor, the Bahr el Zeraf ("Sea of the Giraffes") river branches off the Bahr al Jabal to the east, diverting part of the flow, and again joins the Bahr al Jabal just before reaching Malakal. During the course of its flow, the Bahr al Jabal passes Lake No, where the Bahr el Ghazal ("Sea of the Gazelles") connects to the Bahr al Jabal, contributing an inflow with seasonal variation. At Malakal, the Sobat River joins into the system. The combined flows then stream to the north as the White Nile in a defined bed, joining with the Blue Nile waters at Khartoum to form the main Nile. Sudd was designated as a Ramsar Wetland of International Importance on 5 June 2006. An area of was designated. 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「sudd」の詳細全文を読む スポンサード リンク
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