Examples of using Surface currents in English and their translations into Indonesian
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Ecclesiastic
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Ecclesiastic
And the red are the warm surface currents.
Surface currents are the most obvious type of current. .
It then rises to replace the water that surface currents constantly carry toward the poles.
Surface currents can extend to depths of about 65 feet(20 meters).
Ocean currents such as the Gulf Stream are wind-driven surface currents. .
The two main types of ocean currents are surface currents and deep water or bottom currents. .
As surface currents move, they absorb heat in the tropical regions and release it in colder environments near the poles.
This deflection, combined with the rotation of Earth on it axis, forces surface currents to flow in circular patterns.
Surface currents, which are about 400 meters on the top part of ocean, account for about 10% of the water while deep water currents….
When water moves in this way,other water flows in to fill the gap and a circular movement of surface currents known as a gyre is formed.
When NASA made a visualization of ocean surface currents around the world the result looked remarkable like the 1889 work of the celebrated Van Gogh.
When water moves in this way,other water flows in to fill the gap and a circular movement of surface currents known as a gyre is formed.
Surface currents are formed by the friction of waves produced by the wind and by tides, the changes in local sea level produced by the gravity of the Moon and Sun.
By combining their measurements with a computer model of ocean circulation, theresearchers report that this concentration of plastic occurred in an area where wind-driven surface currents were converging.
Surface currents only affect the top few hundred meters(yards) of the sea, but there are also large-scale flows in the ocean depths caused by the movement of deep water masses.
But they can survive for long periods in saltwater without eating or drinking,so by only traveling when surface currents are favorable, they would be able to move long distances by sea.".
Surface currents in the Alboran Sea, influenced by the prevailing winds, flow eastward, bringing water from the Atlantic into the Mediterranean; deeper subsurface currents flow westward, carrying saltier Mediterranean water over the Gibraltar sill into the Atlantic.
To create the model, Jönsson andWatson obtained surface-current data from a database of modeled global surface currents developed at the Massachusetts Institute of Technology and housed at NASA's Jet Propulsion Laboratory in California.
Surface currents are formed in response to wind patterns, but deep ocean currents that move more of the planet's heat follow courses that are more related to the bathym etry(topography of the seafloor) and the spinning of the Earth than they are related to surface winds.
And so… dive and let the surface current pull us through the Strait.
The sea surface current at our location is 2-2.3 knots in the direction of 225-230.
Water flows in both directions along the strait, from the Sea of Marmara to the Aegean via a surface current and in the opposite direction via an undercurrent.
Although winds are variable, in any oneplace they predominantly blow from a single direction and thus a surface current can be formed.
Where high frequency currents are considered, with skin effect, the surface current densities and magnetic field may be obtained by solving the Laplace equation.
Although winds are variable, in any one placethey predominantly blow from a single direction and thus a surface current can be formed.
The then-weaker surface current will impose less friction and drag on the EUC, so this deeper current will strengthen by 14 percent.
Energy moves towards the sun's surface through convection currents of heated and cooled gas.
River currents are visible from the surface; however currents that occur in the sea are not as visible on the surface.