Examples of using Tidal flow in English and their translations into Malay
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Colloquial
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Ecclesiastic
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Computer
The reintroduction of tidal flow to restore mangrove and tidal marsh ecosystems has been identified as the most promising potential activity.
Restricts"lagoon" to bodies of water with little or no fresh water inflow,little or no tidal flow, calls any bay that receives a regular flow of fresh water an"estuary".
For land-based facilities that discharge into the marine environment, such as sewage treatment plants or settlement pond overflows, there might be options for holding wastewater until conditions have easedfor corals, or at least discharging when mixing potential is greatest(e.g., large tidal flows).
These policies might involve replanting seagrass meadows,reintroducing tidal flow to restore mangroves or preventing potential losses caused by coastal development.
Richard A. Davis Jr. restricts"lagoon" to bodies of water with little or no fresh water inflow,and little or no tidal flow, and calls any bay that receives a regular flow of fresh water an"estuary".
A tidal bore is a surge of tidal origin, which means there is abrupt changes in flow depth.
Among the issues raised in the seminar Q&A sessions were the choice of the GCMs used in the study, the boundary conditions for dynamical downscaling,the inclusion of tidal effects in studies on projected future flows in flat terrains, and the various applications of the climate impact study in planning and development. There were also confusion regarding the terms‘forecast' and‘projection'.
A abrupt increase in flow depth is called a positive surge, which leads to the formation of a tidal bore.
The proposed designs range from preserving the rustic, reflecting tidal rythm, promotiong well-being, vibrancy, pulse of life, discovering culture, molding forms, inspired by nature to streamlined flow.
Wind direction- The tidal bore will be smaller is it is flowing against a strong wind due to the effect of air pressure on the water.
A tidal bore is a rare natural phenomenon in which an incoming tide creates a wave of water that travels up along a river or a narrow bay causing water to flow against the river's current.