Thermohaline circulation is also called overturning circulation. It is driven by density. The time scale for thermohaine is 1000 years.
is called the "ocean".
The type of surface that warms up the slowest is the "ocean" surface.
The surface of the Earth is called the "crust" which is geological terms is the outermost layer of planet or satellite. In the case of the Earth, the crust is composed of igneous, metamorphic and sedimentary rocks and is about 20miles to 50miles thick on the continent and about 3 to 6miles thick in the ocean.
i believe roughly 70% (not completely sure though) I'm not really sure, but something like 70% of the earths surface..
In order for temperature to change the involved heat has to have some place to go. The water at the bottom of the ocean is surrounded by ground and other water that are already at the same temperature. Where can extra heat go to? At the surface the air transports heat up and away so ocean heat can leak out (or in) to the water.
The Great Ocean Conveyor Belt is also called thermohaline circulation.
Global Ocean Conveyor
The term thermohaline circulation ( THC ) refers to the part of the large-scale ocean circulation that is driven by global density gradients created by surface heat and freshwater fluxes
Thermohaline circulation is driven by changes in temperature and salinity of ocean water. Cold, dense water sinks in the polar regions due to its high salinity and low temperature, driving the deep ocean currents that help regulate the global climate by redistributing heat and nutrients around the world.
thermohaline circulation
Thermohaline circulation is a global pattern of ocean currents driven by differences in temperature and salt concentration. It plays a crucial role in distributing heat around the planet and regulating climate. This circulation helps transport nutrients and oxygen throughout the ocean, influencing marine ecosystems.
Another name for thermohaline circulation is the ocean conveyor belt. This circulation pattern involves the movement of water around the world's oceans based on differences in temperature and salinity.
thermohaline
Deep ocean currents are primarily driven by two main forces: thermohaline circulation and wind. Thermohaline circulation is influenced by variations in water density, which is affected by temperature (thermo) and salinity (haline). As surface water cools and becomes saltier, it sinks, creating a global conveyor belt of deep ocean currents. Additionally, wind-driven surface currents can also influence deeper currents through the process of upwelling and downwelling.
The driving force of deep-ocean circulation is primarily the sinking of cold, dense water at high latitudes due to its higher density. This process is known as thermohaline circulation, where temperature and salinity differences create variations in water density, causing water masses to sink and drive the global ocean circulation.
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.
Deep ocean circulation(90% of ocean water) is caused by differences in temperature, salinity and suspended load. It is referred to as "Thermohaline"- meaning heat and salt- circulation.