In areas where wind belts converge I'd say, considering they aren't limited to JUST storms.
Human activities such as mining, pollution, minerals processing, landfills, etc have an effect on the flow pattern.
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Effect of pollution</h3>
It should be noted that pollution is usually difficult to control because it is often the result of human infrastructure around a river.
For example, sewage and effluent are discharged into rivers in some areas and this can lower the pH of the water, and hence affect the organisms.
Also, human activities such as mining, pollution, minerals processing, landfills, impact negatively on the quality of water and the flow pattern in the upper reaches of the blood river in Limpopo.
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Answer:
Ghana is a country in the Western region of Africa. Its geography is divided into four major zones.
The coastline which is sandy with plains and scrub with rivers and streams.
The high plains are found in the northern part of Ghana.
Ashanti uplands and plateau which are found in the South-west and south-central part of Ghana
The hilly Akwapim-Togo ranges are found along Ghana's eastern international border.
These features makes the country distinct.
Explanation:
In the equatorial region, the oceans are heated more than in the polar regions. This is due to the way the sun rays ‘hit’ the different latitudes of earth due to its spherical nature. Due to their higher temperatures, they are less dense. In addition due to the fact that water at higher temperatures can dissolve more salts, the oceans at the equator are less concentrated with salts per volume compared to ocean water in the polar region.
In the poles, water is cooler and hence denser. Due to the low temperatures, the water can accommodate fewer salts hence the ocean waters have a higher salt concentration per volume.
The ocean currents from the equatorial region flow towards the poles on the surface of the oceans while the ocean's currents from the poles towards the equator flow on the bottom of the oceans because they are denser from the higher salinity concentrations and low temperatures.
When the polar current reaches the equatorial region, they upwell to replace the warmer currents moving towards the poles. The currents warm-up, become less dense and less concentrated with salts. The warm currents moving towards the polar region get cooler and denser. They also become more concentrated with salts and some of it precipitates to the bottom of the oceans when saturation point is reached.
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