Thermohaline circulation is a global system of ocean currents driven by differences in water temperature (thermo) and salinity (haline). These differences affect water density, causing colder, saltier water to sink and warmer, fresher water to rise. This process creates a vast "conveyor belt" that moves water, heat, and nutrients around the planet, playing a crucial role in regulating Earth's climate and supporting marine life in oceans and seas.
Thermohaline circulation is a global system of ocean currents driven by differences in water temperature (thermo) and salinity (haline). These differences affect water density, causing colder, saltier water to sink and warmer, fresher water to rise. This process creates a vast "conveyor belt" that moves water, heat, and nutrients around the planet, playing a crucial role in regulating Earth's climate and supporting marine life in oceans and seas.
What is thermohaline circulation?
A global ocean circulation driven by density differences from surface temperature (thermo) and salinity (haline); it moves water around the world as part of the meridional overturning system.
How is deep water formed in this circulation?
Cold, salty water becomes dense and sinks in polar regions, initiating deep-water currents that drive the global overturning.
How do temperature and salinity affect thermohaline circulation?
Colder temperatures and higher salinity increase water density, promoting sinking; warmer or fresher water reduces density and can weaken the overturning.
Why is thermohaline circulation important for climate?
It redistributes heat and nutrients across oceans, influencing regional climates and weather patterns; changes in its strength can impact global climate.