| • वेलांचली परिवहन | |
| transport: ढुलाई माल वाहक | |
longshore transport मीनिंग इन हिंदी
longshore transport उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- Beaches further south provide nourishment to the northern coast via longshore transport.
- Longshore currents can generate oblique breaking waves which result in longshore transport.
- This means that longshore transport mainly occurs in the nearshore swash zone.
- This drop in sediment yield has inevitably altered the longshore transport equilibrium in the local coastal area.
- The wave interaction model assumes that two edges of waves interact, create differing wave heights, and cause longshore transport of nearshore currents.
- Sediment removed from the cliffs, brought onshore from offshore and the sediment supplied by rivers that remains in the lower foreshore zone undergoes longshore transport.
- Reasons can include : seawalls locking up sand dunes, coastal structures like ports and harbors that prevent longshore transport, dams and other river management structures.
- The Boundary Interaction Model assumes that the topography of the sea bottom causes nearshore circulation and longshore transport; the result of both models is a rip current.
- The system underwent further changes c . 500 year BP, when longshore drift from the eastern end of the spit system created the barrier, which has been retained due to ongoing longshore transport.
- In the Northern Zone however, from Taumutu to Birdlings Flat / Banks Peninsula conditions are relatively stable as longshore transport into the zone is small, but sufficient to maintain a relative equilibrium ( Kirk, 1967 ).
