longshore current वाक्य
उदाहरण वाक्य
मोबाइल
- Longshore currents can generate oblique breaking waves which result in longshore transport.
- Longshore currents have deposited beach ridges since then for 6, 000 years.
- Longshore currents flow parallel to the beaches, making waves break obliquely on the sand.
- Longshore currents also commonly create offshore bars, which give beaches some stability by reducing erosion.
- This coastline is characterised by its mixed sand and gravel beaches and southerly longshore currents.
- It may have been swept southward by longshore currents from an eroding sandstone terrain in Canada.
- The combination of large swells, high tide, and powerful south-to-north longshore currents impeded by the Newport Beach.
- Rivers, waves, and longshore currents segregate mud, silt, and clay from sand and gravel due to fall velocity.
- The tombolo model affirms a constant sediment source and a high unidirectional or bi-directional ( monsoonal ) longshore current.
- Sediment that remains in suspension when the following wave crest arrives will not be able to settle and compact and will be more susceptible to erosion by longshore currents and receding tides.
- Skagen Odde is reported to be one of the largest spit systems in Europe, created by a continuous process of marine sand and gravel deposition, moved in a north-east direction by longshore currents.
- On intermediate states with pronounced bar-trough ( straight or crescentic ) topographies, incident wave orbital velocities are generally dominant but significant roles are also played by subharmonic and infragravity standing waves, longshore currents, and rips.
- Cape Fear is formed by the intersection of two sweeping arcs of shifting, low-lying beach, the result of longshore currents which also form the treacherous, shifting Frying Pan Shoals, part of the Graveyard of the Atlantic.
- Coastlines facing very energetic wind and wave systems will tend to hold only large rocks as smaller particles will be held in suspension in the turbid water column and carried to calmer areas by longshore currents and tides.
- This is often required where the flow of new sediment caused by the longshore current has been disrupted by construction of harbors, breakwaters, causeways or boat ramps, creating new current flows that scour the sand from behind these structures, and deprive the beach of restorative sediments.
- Higher energy waves breaking in quick succession tend to mobilise sediment from the shallows, keeping it in suspension where it is prone to be carried along the beach by longshore currents, or carried out to sea to form longshore bars, especially if the longshore current meets an outflow from a river or flooding stream.
- Higher energy waves breaking in quick succession tend to mobilise sediment from the shallows, keeping it in suspension where it is prone to be carried along the beach by longshore currents, or carried out to sea to form longshore bars, especially if the longshore current meets an outflow from a river or flooding stream.
- But the sand keeps flowing, carried not only by waves but also by a longshore current of sorts called a littoral drift . To keep sand from closing the inlets, people build groins jutting out into the ocean, on the up-current side of the littoral drift . And sure enough, the inlet stays open because sand piles up on the up-current side of the groin.
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