7.1
breakwaters Constructed at the entrances to rivers,
they extend into the ocean in order to stabilise river entrances and provide
safe access for boating by keeping the river entrance clear of sand build-up.
However, these breakwaters can act to dramatically alter patterns of erosion,
transportation and deposition of sand along the coastline.
silting - will make the beaches have lower depth and
may close off some beaches like fresh water en which they have a narrow opening
tidal flushing - action of saltwater entering an
estuary twice a day during the high tides. It renews the salinity and nutrients
to the estuary and removes artificially introduced toxins in the environment.
sea change the phenomenon of increasing
migration to, and suburbanisation of, any coast, particularly those areas
outside the primary urban metropolitan centres
urban stormwater the stormwater from urban areas will
go to the sea so if they are polluted then so is the sea
dredging is an excavation activity or operation
usually carried out at least partly underwater, in shallow seas or fresh water
areas with the purpose of gathering up bottom sediments and disposing of them
at a different location. This technique is often used to keep waterways
navigable.
introduced plants introduced plants are plants that
aren't native to that nation and will usually take over the native population.
7.2
ground swell - a broad, deep swell or rolling of the
sea, due to a distant storm or gale.
plunging waves - Break on beaches where the slope is
moderately steep. Board riders like these waves because of the tubes they form
spilling waves - Break far from the shore on beaches
with gentle slopes. The surf (white foam) gently rolls over the front so these
waves are good for body surfing
surging waves - Occur on very steep beaches. The waves
roll up the steep face rather than breaking over it. They cause erosion.
wind swell - In fluid dynamics, wind waves or, more
precisely, wind-generated waves are surface waves that occur on the free
surface of oceans, seas, lakes, rivers, and canals or even on small puddles and
ponds. They usually result from the wind blowing over a vast enough stretch of
fluid surface.wave height the height of waves
wavelength the distance between waves
fetch the distance that wind travels over the ocean to
form waves
surf and swash zonethe active part of the
coast in terms of erosion and deposition of sand by wave action; the surf zone
is immediately adjacent to the coast and the swash zone is at the shore once
the waves have broken
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