In the ocean, water temperature generally decreases with increasing depth due to the absorption of sunlight by the surface layer, which warms it. This phenomenon creates distinct thermal layers, with the warmest water found near the surface and a rapid drop in temperature occurring in the upper few hundred meters, known as the thermocline. Below the thermocline, temperatures stabilize and remain cold, often near freezing in the deep ocean.
The temperature goes down ie it gets colder.
A rapid change in temperature with depth in the ocean is called thermocline. A rapid change in density with depth in the ocean is called the pynocline.Thermocline
The density of the water increases with the salinity, so saline water is denser and sinks to the bottom. Temperature is also a factor, however. Cold, saline water is the densest
A rapid change in ocean density with depth is called a thermocline. This thermocline is caused by variations in temperature and can impact ocean circulation and marine life distribution.
As you descend into the ocean, temperature typically decreases due to the lack of sunlight penetration and heat exchange with the cold deep water. Pressure, on the other hand, increases with depth due to the weight of the water above pushing down.
the density of sea increases with depth
As wer gets deeper there is less oxygen and it gets colder.
As ocean depth increases, pressure also increases. This is because as water depth increases, there is more water above exerting force due to gravity. Pressure in the ocean increases about 1 atmosphere (atm) for every 10 meters of depth.
the pressure increases i forgot why but that's what i know
Its intensity decreases.
The term you are referring to is "thermocline." It is the layer of water in the ocean where there is a rapid change in temperature with depth, serving as a barrier between warmer surface water and colder deep water.
Well as you go further down into the ocean, it will be colder. Usually but not always!! Temperature and salinity affect the density of seawater, and in many systems, density increases with depth (as temperature decreases and salinity increases). IT is however possible to observe patterns where dense water at depth is either very salty but warm, or very cold, but nearly fresh.