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1.
What is a tide ?
Ans: A tide is the periodic rise and fall in
the height of the surface of the water. A fall
in tide may be the reason you cannot get your
boat off the beach in the morning.
2.
What is a tidal stream ?
Ans:
A
tidal stream is the horizontal flow of water
that results from tides. A strong tidal stream
is often experienced in the Gippsland Lakes
near Lakes Entrance. A tidal stream is one of
the reasons why your speed over the ground may
differ to your speed through the water. You
could be going backwards.
3.
What is a current ?
Ans:
Currents result from the large scale
circulation of the worlds oceans.
4.
What is the cause of a tide ?
Ans:
The primary influence is the gravitational
effect of the moon. Since the earth is
spinning once every 24hours the highs (and
corresponding lows) produce a tidal pattern
involving 2 high and 2 low tides each day.
5.
Why isn't the high tide at the same time every
day ?
Ans: The moon orbits the earth each lunar
month. The tide pattern is repeated over a
lunar day of 24 hours and 52 minutes. Tide
times move back an hour a day.
6.
Why do the highs and lows differ ?
Ans: The latitude of the moon varies over the
lunar month. When the moon is directly over
the equator the 2 highs and the 2 lows will be
equal. This happens fortnightly.
7.
What are spring and neap tides ?
Ans: Twice every lunar month the sun and moon
will work together to produce very high
(spring) and very low (neap) tides. The highs
will be at new moon and at full moon. 7 days
later the sun and moon will work against each
other to produce neap tides. This will be
around the first and the third quarters. Neap
tides will produce weak tidal steams.
8.
What is a king tide ?
Ans: A king tide is just the highest of the
high tides. They generally occur around
Christmas in daylight hours and in winter at
night.
9.
What else affects water heights ?
Ans:
At
sea the shape of the land mass will effect the
tidal influences. The influence can be so
great that there is only 1 high and 1 low per
day as at Karumba in the Gulf of Carpentaria.
In partially enclosed waters the major
influence may be meteorological. At Goolwa the
water level can drop several feet as water is
blown into Lake Alexandria and Lake Albert. A
less pronounced effect can occur at the
Gippsland Lakes and can result in a stream
running (up) into Lake Wellington. This has
apparently happened during some of the Marley
races. It is said that in light conditions
some skippers have blissfully sailed backwards
whilst others have gained on the fleet by
anchoring. At Lake Macquarie a major influence
is barometric pressure. Low pressure systems
raise sea levels, high pressure systems lower
them. Take to the hard to avoid bad weather
and you might be stuck there until the next
bad weather. An intense cyclone can raise the
sea level by greater than 2 metres.
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