The Gulf Stream Flows Clockwise—A Warm River in the Atlantic

The Gulf Stream is a warm, swift western boundary current forming the North Atlantic Subtropical Gyre's western limb. Its path traces a massive clockwise loop:

1. Florida Current: Narrow, intense flow through the Straits of Florida (5–6 knots, 30 Sv)
2. Gulf Stream proper: Northeastward along the U.S. East Coast, peeling eddies
3. North Atlantic Current: Broad, diffuse eastward flow toward Europe
4. Azores Current / Canary Current: Southward along Africa, closing the gyre
5. North Equatorial Current: Westward across the tropical Atlantic, feeding back into the Caribbean and Gulf of Mexico

Climate Engine

The Gulf Stream transports ~1.3 petawatts of heat poleward—equivalent to millions of power plants. It warms Western Europe (London is 5°C warmer than Newfoundland at the same latitude), fuels nor'easters, and modulates hurricane intensity.

Not a River, But a Dynamic Feature

Its path meanders; eddies pinch off; strength varies seasonally and decadally. Climate change may weaken it (AMOC slowdown), with profound implications for regional climate and sea level.

Clockwise. Warm. Powerful. The Gulf Stream is the Atlantic's heartbeat.