Q.How is the movement of currents influenced by prevailing winds? Give some examples from Figure 13.3.

Think of a fan blowing across a bowl of water. The surface doesn't stay still — it gets pushed into little ripples and currents that follow the direction of the breeze. Now scale that bowl up to the size of an entire ocean, and the breeze becomes the planet's prevailing winds, blowing steadily across thousands of kilometres. That push is the single most powerful engine for moving surface water on Earth, and the currents it creates are what we call wind-driven ocean currents.

The intuition is simple: wind drags the water's surface. But the ocean doesn't just slide along in a straight line. Because the Earth spins, anything moving over its surface — air or water — gets deflected sideways. In the northern hemisphere, moving water bends to the right; in the southern hemisphere, it bends to the left. This is the Coriolis effect, and it turns a straightforward push into a spiral. The surface water moves at about 45° to the wind direction, and each layer below moves a little slower and a little more to the side, until the motion fades out at depth. That stacked, twisting pattern is called the Ekman spiral, and its net effect — the average movement of the whole top layer — is at right angles to the wind. So a wind blowing from the east doesn't push water west; it pushes it north or south, depending on which hemisphere you're in.

That might sound like a technical curiosity, but it explains some of the most visible features on a world map. The great gyres — those giant circular flows in the Atlantic, Pacific, and Indian Oceans — are wind-driven. The trade winds blow from the east near the equator, the westerlies blow from the west at mid-latitudes, and together they spin the ocean surface into enormous clockwise loops in the north and counter-clockwise loops in the south. The Gulf Stream, which carries warm water up the east coast of North America and across the Atlantic to warm western Europe, is one arm of the North Atlantic gyre. It is not a river in the ocean; it is a wind-driven conveyor belt, and its warmth is why winters in Britain are far milder than those in Labrador at the same latitude.

Why does this matter beyond geography class? Because wind-driven currents redistribute heat. They carry warm water from the tropics toward the poles and cold water back toward the equator, moderating climates on every continent. They also steer marine life: plankton, fish larvae, and nutrients travel with the currents, so the same winds that move water also shape where fisheries thrive and where coastlines erode. And for anyone studying trade, commerce, or history, these currents were the original highways — sailing ships followed them, and the routes of the old spice trade, the transatlantic slave trade, and colonial shipping all trace the paths of wind-driven water. …