The Atlantic Ocean's temperature varies dramatically by latitude, depth, and currents—ranging from near-freezing at the poles to bathtub-warm in the tropics.
Sunlight penetrates only the upper ~200 m (euphotic zone). Below the thermocline, temperatures drop steadily; the abyssal plain hovers around -1°C to 4°C (30–39°F).
The Gulf Stream transports warm water northeast, moderating Western Europe's climate. The Canary Current and Benguela Current bring cooler water equatorward on eastern boundaries.
Temperature dictates species distributions, coral bleaching thresholds, hurricane fuel, and global heat redistribution. Monitoring Atlantic thermal structure is critical for climate models and fisheries management.