Nonlinear effects of wind on Atlantic ocean circulation

The Atlantic Meridional Overturning Circulation (AMOC) is a system of ocean currents that transports warm, salty water from the tropics to the northern Atlantic. As the water cools, it becomes denser and sinks, in a process known as overturning. The cold deep water then flows back toward the equator. This process of transportation plays a critical role in Earth
The Atlantic Meridional Overturning Circulation (AMOC) is a system of ocean currents that transports warm, salty water from the tropics to the northern Atlantic. As the water cools, it becomes denser and sinks, in a process known as overturning. The cold deep water then flows back toward the equator. This process of transportation plays a critical role in Earth's climate.

The Gulf Stream has increased steadily over the last century

Atlantic meridional overturning circulation increases flood risk along the United States southeast coast

Wind-current feedback is an energy sink for oceanic internal waves

Global forestation and deforestation affect remote climate via adjusted atmosphere and ocean circulation

How would temperatures change in Europe if the Gulf Stream shut down? : r/geography

Wind-Driven Circulation - an overview

Atlantic meridional overturning circulation - Wikipedia

Short-term, linear, and non-linear local effects of the tides on the surface dynamics in a new, high-resolution model of the Mediterranean Sea circulation