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The flow of water from upstream DKI transferred to Flood Canal directly into the sea
flow in the area of South Jakarta with the contour of the ground high enough to flow by gravity
in the northern part of the low-flow water is managed by a system of polders (dykes, reservoirs and pumps).
The upstream / south need to be built / preserved lakes, reservoirs and reforestation to resist the flow of water to Jakarta.
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