Question

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Answer 1

Answer:

1- HALOCLINE

2- WIND

3- DISSOLVED INORGANIC SALT

4- IONIC COMPOUND

5- CORIOLIS EFFECT

Explanation:

Halocline is a vertical zone in the water body in which the salinity changes gradually with respect to the depth. It is the region that lies below the mixed layer. The presence of this layer helps in the formation of sea ice and also does not allow the Carbon dioxide to release into the atmosphere.

Ocean waves are generated due to the friction between the wind and the surface of the ocean. This are known as the wind-driven waves or the surface waves.

Salinity is usually defined as the amount of dissolved inorganic salt present in the seawater. These salts are ionic compounds and when it gets dissolved in water, it splits completely into the ions. The two ions namely the sodium and chlorine combines with each other to form sodium chloride (NaCl).

The trade winds are blown from the northeastern to southwestern side in the northern hemisphere and southeast to the northwestern side in the southern hemisphere. Both the trade winds converges along the equatorial region forming the Inter-Tropical Convergence zone. When these winds blows it gets deflected due to the effect of Coriolis force. This force generates due to the earth's rotation.

Answer 2

Answer:

Explanation:

halocline

wind

dissolved salts

ionic

Coriolis

Convection currents flow due to variations in the temperature and salinity in seawater, which both influence its density. Variations in density in different regions of the ocean will cause water to flow from less dense areas to more dense areas as water heats up and becomes less saline, producing a horizontal convection current. Vertical convection currents can arise as cooler, more saline water sinks, causing warmer, less saline water to rise.