The global current conveyor belt begins on the surface of the ocean near the pole in the North Atlantic.
thermohaline circulation
The global current conveyor belt begins in the North Atlantic Ocean, where warm water from the Gulf Stream moves northward to the Arctic. This warm water eventually cools and sinks in the Labrador Sea, starting a deep current that travels southward along the ocean floor.
Global climate change could potentially disrupt the global conveyor belt by altering temperature and salinity patterns in the ocean. This could lead to changes in ocean currents and potentially weaken or even shut down parts of the global conveyor belt, impacting global climate systems. This could have far-reaching consequences on weather patterns, marine ecosystems, and even regional climates around the world.
The simplified pattern of ocean currents,looks like a conveyor belt,moving water between the oceans
The global oceanic conveyor belt, is a unifying concept that connects the ocean's surface and thermohaline (deep mass) circulation regimes, transporting heat and salt on a planetary scale.
The Great Ocean Conveyor Belt is also called thermohaline circulation.
You think probable to the differences between sodium chloride concentration in ocean waters.
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The simplified pattern of ocean currents,looks like a conveyor belt,moving water between the oceans
Global Conveyor Belt
The global ocean conveyor belt, also known as the thermohaline circulation, is a system of deep-ocean circulation driven by density differences caused by variations in temperature and salinity. It plays a crucial role in distributing heat around the Earth and regulating climate. Warm surface currents move towards the poles, where they cool, become denser, and sink, forming deep ocean currents that then circulate back towards the equator.