Deep Currents.
Chat with our AI personalities
Temperature, salinity, and density are factors that form thermohaline circulation, which drives the global ocean currents. Temperature affects the water's density, with colder water being denser. Salinity also plays a role, with higher salinity making water more dense. Together, these factors influence the movement of water around the world's oceans.
The two characteristics of water that combine to form a thermohaline current are temperature and salinity. As water becomes cold and more saline, it becomes denser and sinks to the ocean floor, driving the vertical circulation of the ocean known as the thermohaline circulation.
The density of water is 1.0 g/ml2In word form it is one gram per milliliter cubed
Vapor density refers to the density of a vapor compared to the density of air at a given temperature and pressure. It is commonly used to compare the weight of a vapor to an equal volume of air, which can help in understanding how it will disperse in the atmosphere.
A deep current forms when water masses sink and flow horizontally along the ocean floor due to differences in temperature and salinity. This creates a slow-moving, deep-sea current that can transport large amounts of water and nutrients over long distances in the ocean.
the deeper into the ocean you go, the colder the water gets. the water also gets more dense, which means a higher salinity. so in this case, the salinity increases as the temperature decreases. but the surface salinity also increases in areas close to the equator (hotter air). this happens because the water evaporates faster, leaving more salt to a smaller amount of water.