name the three ways in which movement of ocean water takes place
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Answered by
101
Ocean water is moved by three different forces:
1. Waves
2. Currents
3. Tides
Waves:
A wave is a disturbance that transforms energy through matter or empty space. Water waves move ocean water from one place to another.
Currents:
Currents are defined as the large movement of water in the same direction. Currents exist in both temporary and long lasting states. Currents are found on the surface of water and also in the deeper levels of ocean.
Tides:
Tides are the daily changes in the level of the ocean water at any given place. The main factors which cause tides are gravitational pull of the moon and the sun.
1. Waves
2. Currents
3. Tides
Waves:
A wave is a disturbance that transforms energy through matter or empty space. Water waves move ocean water from one place to another.
Currents:
Currents are defined as the large movement of water in the same direction. Currents exist in both temporary and long lasting states. Currents are found on the surface of water and also in the deeper levels of ocean.
Tides:
Tides are the daily changes in the level of the ocean water at any given place. The main factors which cause tides are gravitational pull of the moon and the sun.
Answered by
20
There are distinctive sorts of developments of sea water affected by various physical qualities like temperature, saltiness, thickness, and so forth. Developments of sea water are likewise influenced by outside powers like the sun, moon and the breezes.
The real developments of the sea waters can be ordered into three. They are:
Waves
Tides
Sea Currents
Waves and the sea streams are flat developments of sea waters while the tide is a sort of vertical development of the sea water.
Waves
Waves are only the oscillatory developments that outcome in the ascent and fall of water surface.
Waves are a sort of level developments of the sea water.
They are really the vitality, not the water thusly, which moves over the sea surface.
This vitality for the waves is given by the breeze.
In a wave, the development of each water molecule is in a round way.
A wave has two noteworthy parts: the raised part is called as the peak while the low-point is called as the trough.
Tides
Tide are the periodical ascent and fall of the ocean levels, here and there a day, caused by the joined impacts of the gravitational powers applied by the sun, the moon and the revolution of the earth.
They are a vertical development of waters and are not the same as developments of sea water caused by meteorological impacts like the breezes and air weight changes.
Note: The water developments which are caused by the meteorological impacts like the said above are called as surges and they are not normal like tides.
The moon's gravitational draw, as it were, is the significant reason for the event of tides (the moon's gravitational fascination is more viable on the earth than that of the sun).
Sun's gravitational draw and the diffusive power because of the pivot of earth are alternate powers which act alongside the moon's gravitational force.
Sea Currents
The sea streams are the flat stream of a mass of water a genuinely characterized way finished extraordinary separations.
They are much the same as a stream streaming in a sea.
Sea streams can be shaped by the breezes, thickness contrasts in sea waters because of contrasts in temperature and saltiness, gravity and occasions, for example, seismic tremors.
The heading of development of a sea momentum is principally affected by the revolution of the earth (because of Coriolis compel, most sea streams in northern side of the equator move in clockwise way and sea ebbs and flows in southern half of the globe move in an against clockwise way).
The real developments of the sea waters can be ordered into three. They are:
Waves
Tides
Sea Currents
Waves and the sea streams are flat developments of sea waters while the tide is a sort of vertical development of the sea water.
Waves
Waves are only the oscillatory developments that outcome in the ascent and fall of water surface.
Waves are a sort of level developments of the sea water.
They are really the vitality, not the water thusly, which moves over the sea surface.
This vitality for the waves is given by the breeze.
In a wave, the development of each water molecule is in a round way.
A wave has two noteworthy parts: the raised part is called as the peak while the low-point is called as the trough.
Tides
Tide are the periodical ascent and fall of the ocean levels, here and there a day, caused by the joined impacts of the gravitational powers applied by the sun, the moon and the revolution of the earth.
They are a vertical development of waters and are not the same as developments of sea water caused by meteorological impacts like the breezes and air weight changes.
Note: The water developments which are caused by the meteorological impacts like the said above are called as surges and they are not normal like tides.
The moon's gravitational draw, as it were, is the significant reason for the event of tides (the moon's gravitational fascination is more viable on the earth than that of the sun).
Sun's gravitational draw and the diffusive power because of the pivot of earth are alternate powers which act alongside the moon's gravitational force.
Sea Currents
The sea streams are the flat stream of a mass of water a genuinely characterized way finished extraordinary separations.
They are much the same as a stream streaming in a sea.
Sea streams can be shaped by the breezes, thickness contrasts in sea waters because of contrasts in temperature and saltiness, gravity and occasions, for example, seismic tremors.
The heading of development of a sea momentum is principally affected by the revolution of the earth (because of Coriolis compel, most sea streams in northern side of the equator move in clockwise way and sea ebbs and flows in southern half of the globe move in an against clockwise way).
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