• The ocean is in constant motion. You can see this for yourself when you watch waves crash onto shore. If you go swimming, you may even feel an ocean current pulling you along. Surface currents, such as the Gulf Stream, move water across the globe like mighty rivers. Surface currents are powered by the Earth’s various wind patterns.

    The ocean also has deep underwater currents. These are more massive but move more slowly than surface currents. Underwater currents mix the ocean’s waters on a global scale. A process known as thermohaline circulation, or the ocean conveyor belt, drives these deep underwater currents.

    Thermohaline Circulation

    Thermohaline circulation moves a massive current of water around the globe, from northern oceans to southern oceans, and back again. Currents slowly turn over water in the entire ocean, from top to bottom. It is somewhat like a giant conveyor belt, moving warm surface waters downward and forcing cold, nutrient-rich waters upward.

    The term thermohaline combines the words thermo (heat) and haline (salt), both factors that influence the density of seawater. The ocean is constantly shifting and moving in reaction to changes in water density. To best understand ocean water dynamics, or how water moves, there are a few simple principles to keep in mind:

    • Water always flows down toward the lowest point.
    • Water’s density is determined by the water’s temperature and salinity (amount of salt).
    • Cold water is denser than warm water.
    • Water with high salinity is denser than water with low salinity.
    • Ocean water always moves toward an equilibrium, or balance. For example, if surface water cools and becomes denser, it will sink. The warmer water below will rise to balance out the missing surface water.


    Ocean Layers

    The ocean can be divided into several layers. The top layer of the ocean collects the warmth and energy of sunlight, while the bottom layers collect the rich, nutrient-filled sediment of decayed plant and animal matter.

    The top ocean layer is about 100 meters (330 feet) deep. Enough sunlight reaches that depth for organisms, such as phytoplankton, to carry out photosynthesis. Phytoplankton makes up the first part of the marine food chain and is essential to all ocean life.

    The middle, or barrier, layer is called the thermocline. The ocean’s temperature and density change very quickly at this layer. The barrier layer is about 500 to 1,000 meters (1,600 to 3,300 feet) deep.

    Below the barrier layer is the bottom layer, referred to as the deep ocean. It averages about 3 kilometers (2 miles) in depth.

    The Conveyor Belt

    Scientists have long understood how nutrients move from the ocean’s surface to its depths. As phytoplankton die, they sink and collect on the ocean floor. But if nutrients are continually sinking to the depths of the ocean, how are surface waters replenished with nutrients? Scientists discovered that in certain regions of the ocean, the nutrient-rich deep water was upwelling, or rising to the surface.

    Scientists realized that the ocean was slowly turning over from top to bottom in a continuous global loop. Like a conveyor belt, thermohaline circulation moves nutrients from one part of the ocean to another.

    Let’s start in the northern Atlantic Ocean and follow the conveyor belt as it moves water around the Earth.

    In the seas near Greenland and Norway, the water is cold. Some of it freezes, leaving salt behind. The cold, salty water becomes dense and sinks to the ocean floor. This water is known as the North Atlantic Deep Water, and it is one of the primary driving forces of the conveyor belt.

    The force of the sinking cold water pushes the existing North Atlantic Deep Water south, toward Antarctica, in a slow-moving underwater current. When it reaches Antarctica, the water flows east with the Antarctic Circumpolar Current, a massive and powerful current that circles the continent.

    Parts of the Antarctic Circumpolar Current flow northward and move into the Indian and Pacific Oceans. As the deep, cold water travels through the oceans, it mixes with warmer water. The water eventually becomes warm enough to rise, creating a slow upwelling that brings nutrients to the surface.

    In the Pacific, the surface water flows through the Indonesian islands into the Indian Ocean, around southern Africa, and back into the Atlantic. The warm waters eventually travel back to the North Atlantic Deep Water, completing the global loop.

    It takes about 500 years for the conveyor belt to turn over the ocean’s waters and make one complete trip around the Earth.

    The North Atlantic Deep Water

    The deep water in the Greenland Sea flows along toward the lowest point on the floor of the North Atlantic Ocean. The water collects in a basin, the same way river water flows into a lake or pond. The basin is the North Atlantic Deep Water.

    Other seas feed their cool ocean waters into the North Atlantic Deep Water. In the Labrador Sea, off the coast of northeastern Canada, the cold water sinks to depths of 3,000 meters (9,900 feet) at a rate of 10 centimeters (about 4 inches) per second.

    Another source of the North Atlantic Deep Water is the Mediterranean Sea. As the warm surface water of the Mediterranean evaporates, the water grows saltier and denser. This water exits the Mediterranean through the Strait of Gibraltar, the narrow channel between Spain and Morocco that connects the sea to the Atlantic Ocean. The Mediterranean’s deep water pours into the Atlantic at a rate of 2 meters (about 6.5 feet) per second and helps raise the overall salinity of the Atlantic Ocean.

    The Antarctic Circumpolar Current

    When the conveyor belt reaches the southern part of the globe, it is driven back to the northern oceans by the Antarctic Circumpolar Current.

    Western winds are very strong in the Antarctic. They help create the intensely powerful Antarctic Circumpolar Current. The current moves a lot of water very quickly around the continent of Antarctica—about 140 million cubic meters (4.9 billion cubic feet) of water per second.

    Overturning occurs in the waters around Antarctica. Overturning happens when the extremely frigid Antarctic surface water sinks. This forces the nutrient-rich deep water to rise. Overturning moves massive amounts of water. An estimated 35 to 45 million cubic meters (between 1.2 and 1.5 billion cubic feet) of water per second are continually moved from the ocean bottom to the surface in a massive tumbling rotation.

    The Antarctic Circumpolar Current and overturning make the waters around Antarctica an ideal habitat for many marine mammals. Many types of whales, for instance, migrate to the waters around Antarctica every year to feed on phytoplankton and other tiny sea creatures churned up by overturning waters.

    Climate Change

    Ocean temperature plays a key role in the conveyor belt, so a change in the Earth’s climate might have drastic effects on the system. If one part of the conveyor belt breaks down—if cold water is not lifted to the surface in upwelling, for instance—nutrients will not be distributed to start the food chain. Organisms, such as phytoplankton, need those nutrients to thrive. Severe climate change slows phytoplankton from forming the first link in the marine food chain. If the first link is threatened, all life in the oceans is threatened.

    ocean conveyor belt
    Thermohaline circulation takes ocean water on a trip around the world.

    Antarctic Circumpolar Current
    The Antarctic Circumpolar Current moves 140 million cubic meters (4.9 billion cubic feet) of water per second around Antarctica. That single current moves more water than all the rivers on the planet combined. The world's rivers move 1.3 million cubic meters (46 million cubic feet) of water per second.

  • Term Part of Speech Definition Encyclopedic Entry
    basin Noun

    a dip or depression in the surface of the land or ocean floor.

    Encyclopedic Entry: basin
    channel Noun

    waterway between two relatively close land masses.

    Encyclopedic Entry: channel
    climate Noun

    all weather conditions for a given location over a period of time.

    Encyclopedic Entry: climate
    climate change Noun

    gradual changes in all the interconnected weather elements on our planet.

    Encyclopedic Entry: climate change
    continent Noun

    one of the seven main land masses on Earth.

    Encyclopedic Entry: continent
    current Noun

    steady, predictable flow of fluid within a larger body of that fluid.

    Encyclopedic Entry: current
    decay Verb

    to rot or decompose.

    density Noun

    number of things of one kind in a given area.

    Encyclopedic Entry: density
    equilibrium Noun

    point where pushing forces and pulling forces are in balance.

    evaporate Verb

    to change from a liquid to a gas or vapor.

    food chain Noun

    group of organisms linked in order of the food they eat, from producers to consumers, and from prey, predators, scavengers, and decomposers.

    Encyclopedic Entry: food chain
    frigid Adjective

    very cold.

    Gulf Stream Noun

    warm current that starts in the Gulf of Mexico and travels along the eastern coast of the U.S. and Canada before crossing the North Atlantic Ocean.

    habitat Noun

    environment where an organism lives throughout the year or for shorter periods of time.

    Encyclopedic Entry: habitat
    marine Adjective

    having to do with the ocean.

    massive Adjective

    very large or heavy.

    migrate Verb

    to move from one place or activity to another.

    nutrient Noun

    substance an organism needs for energy, growth, and life.

    Encyclopedic Entry: nutrient
    ocean Noun

    large body of salt water that covers most of the Earth.

    Encyclopedic Entry: ocean
    ocean conveyor belt Noun

    system in which water moves between the cold depths and warm surface in oceans throughout the world. Also called thermohaline circulation.

    Encyclopedic Entry: ocean conveyor belt
    ocean layer Noun

    one of five marine depths: epipelagic, mesopelagic, bathypelagic, abyssopelagic and hadalpelagic.

    photosynthesis Noun

    process by which plants turn water, sunlight, and carbon dioxide into water, oxygen, and simple sugars.

    phytoplankton Noun

    microscopic organism that lives in the ocean and can convert light energy to chemical energy through photosynthesis.

    polar Adjective

    having to do with the North and/or South Pole.

    primary Adjective

    first or most important.

    salinity Noun


    sediment Noun

    solid material transported and deposited by water, ice, and wind.

    Encyclopedic Entry: sediment
    shore Noun


    temperature Noun

    degree of hotness or coldness measured by a thermometer with a numerical scale.

    Encyclopedic Entry: temperature
    thermocline Noun

    level or layer of a fluid depth where temperature changes more rapidly than the fluid either above or below it.

    thermohaline circulation Noun

    ocean conveyor belt system in which water moves between the cold depths and warm surface in oceans throughout the world.

    upwelling Noun

    process in which cold, nutrient-rich water from the bottom of an ocean basin or lake is brought to the surface due to atmospheric effects such as the Coriolis force or wind.

    Encyclopedic Entry: upwelling
    wave Noun

    moving swell on the surface of water.

    wind Noun

    movement of air (from a high pressure zone to a low pressure zone) caused by the uneven heating of the Earth by the sun.