Movement of water due to its high temperature and its salt content
This process creates a type of current known as thermohaline circulation. The sinking of saltier, denser water drives a deep, slow-moving current, while the rising of less salty water leads to surface currents. Thermohaline circulation is important for distributing heat and nutrients in the ocean.
Ocean currents are primarily driven by a combination of wind, temperature, salinity, and the Earth's rotation (Coriolis effect). The wind plays a significant role in creating surface currents, while differences in temperature and salinity drive deeper currents through processes like thermohaline circulation. The Coriolis effect influences the direction of ocean currents based on the Earth's rotation.
The pulmonary circulation (from heart to lungs and back) is shorter than the systemic circulation (from heart to body tissues and back).
Deep currents form near the poles because cold, dense water sinks at the poles due to high salinity and low temperatures. This sinking water sets off a global conveyor belt system known as thermohaline circulation, which drives deep currents towards the equator.
there are both single and double circulatory systems.fish have single ones, and birds have double.in double circulatory system the blood travels trough the heart twice in it's way around the body, while in the single it only goes through the heart once.Answer by FutureLPGAgolferThe answer came from my homework and I got it right, it's the Open system and the Closed system.explain how number of exercises affects the breathing rate?
thermohaline circulation
The Great Ocean Conveyor Belt is also called thermohaline circulation.
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 circulation is also called overturning circulation. It is driven by density. The time scale for thermohaine is 1000 years.
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
The thermohaline circulation is a term for the global density-driven circulation of the oceans. Derivation is from thermo- for heat and -haline for salt, which together determine the density of sea water
The global oceanic conveyor belt, is a unifying concept that connects the ocean's surface and thermohaline (deep mass) circulation regimes, transporting heat and salt on a planetary scale.
Global Ocean Conveyor
Another name for thermohaline current is "conveyor belt," which some call this current of the ocean.
Salinity affects thermohaline circulation by influencing the density of seawater. Higher salinity increases water density, promoting sinking of cold, dense water in polar regions. Temperature influences this circulation by controlling the density of water - colder water is denser and more likely to sink. Both factors work together to drive the global thermohaline circulation system.
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.
The thermohaline circulation is important because it helps distribute heat and nutrients around the globe, influencing climate patterns and marine ecosystems. It plays a crucial role in regulating Earth's climate by transporting warm water towards the poles and cold water towards the equator. Any disruption to this circulation pattern can have far-reaching impacts on weather patterns and ecosystems worldwide.