GEOLOGY

Detailed explanation-1: -These deep-ocean currents are driven by differences in the water’s density, which is controlled by temperature (thermo) and salinity (haline). This process is known as thermohaline circulation. In the Earth’s polar regions ocean water gets very cold, forming sea ice.

Detailed explanation-2: -Dense water sinks below less dense water. This is the principle that drives the deep ocean currents that circulate around the world. A combination of high salinity and low temperature near the surface makes seawater dense enough to sink into the deep ocean and flow along the bottom of the basins.

Detailed explanation-3: -Warming temperatures result in weakened currents. If the water at the poles is not as cold and dense, it simply won’t be able to circulate as well. Additionally, the melting of the Greenland continental ice sheet is pouring freshwater into the salty ocean, again altering the density of the water masses.

Detailed explanation-4: -In these areas, the balance between gravity and Earth’s spin causes geostrophic currents to flow. Deep ocean currents are caused by differences in water temperature and salinity.

Detailed explanation-5: -First, along with temperature, they directly affect seawater density (salty water is denser than freshwater) and therefore the circulation of ocean currents from the tropics to the poles. These currents control how heat is carried within the oceans and ultimately regulate the world’s climate.