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Convection currents describe the rising, spread, and sinking of gas, liquid, or molten material caused by the application of heat. … Tremendous heat and pressure within the earth cause the hot magma to flow in convection currents. These currents cause the movement of the tectonic plates that make up the earth’s crust.
Seafloor spreading and other tectonic activity processes are the result of mantle convection. Mantle convection is the slow, churning motion of Earth’s mantle. Convection currents carry heat from the lower mantle and core to the lithosphere. Convection currents also “recycle” lithospheric materials back to the mantle.
Conduction occurs when a substance is heated, particles will gain more energy, and vibrate more. These molecules then bump into nearby particles and transfer some of their energy to them. This then continues and passes the energy from the hot end down to the colder end of the substance.
The air heats, expands and the pressure drop causes air to rise. … In summary: Convection lowers surface pressure which creates a pressure gradient that tries to correct itself by having Air move from higher pressure to the lower pressure area created by the rising air. This correction in pressure is what we call wind.
As the sun heats the atmosphere at the equator, the air rises. As those warm gases head north, they continue to rise higher in the atmosphere and begin to cool. … This air then travels back to the equator to get heated again creating a convection cell. This convection cell is called a Hadley cell.
It moves away from the poles to low pressure areas with warmer, less dense air. This warm air is pushed up by the buoyant force of the colder denser air. As the warm air rises, it cools, and the convection cell recycles itself, over and over again.
Convection occurs when particles with a lot of heat energy in a liquid or gas move and take the place of particles with less heat energy. Heat energy is transferred from hot places to cooler places by convection. Liquids and gases expand when they are heated. … As a result, the particles take up more volume.
How does convection affect the weather? Convection within the atmosphere can often be observed in our weather. For example, as the sun heats the Earth’s surface, the air above it heats up and rises. If conditions allow, this air can continue to rise, cooling as it does so, forming Cumulus clouds.
During convection, cooler water or air sinks, and warmer water or air rises. This movement causes currents. … These currents move water all around the earth, bringing warm water to cooler areas and vice versa. This redistributes thermal energy and causes changes in the weather.
The core heats up the magma and causes a convection current. When magma comes to the top of the mantle, it pushes against tectonic plates, which are huge slabs of rock which the crust rests on. … The movement of the plates can lead to volcanic eruptions, earthquakes, tsunamis and mountain-range formation.
The convection currents move the plates. Where convection currents diverge near the Earth’s crust, plates move apart. Where convection currents converge, plates move towards each other. The movement of the plates, and the activity inside the Earth, is called plate tectonics .
While conduction seems the more obvious method for heat transfer, convection also occurs in the mantle. The warmer, less dense rock material near the core slowly moves upward. … While the mantle material remains solid, the heat and pressure allow convection currents to move the mantle material.
As tectonic plates slowly move away from each other, heat from the mantle’s convection currents makes the crust more plastic and less dense. The less-dense material rises, often forming a mountain or elevated area of the seafloor.
Thus, conduction occurs between the particles of solids, liquids, and gases that collide into one another. During conduction, heat will always transfer from the hotter to the colder object. Temperature is a reflection of the average kinetic energy of the particles of a substance.
Convection carries heat to the surface of the mantle much faster than heating by conduction. Conduction is heat transfer by collisions between molecules, and is how heat is transferred from the stove to the soup pot.
The transfer of heat because of movement of the molecules of the medium, via mass transfer, is called convection or convection of heat. Water and air are bad conductors of heat. But they do become hot, in spite of being bad conductors. Heat transfer in fluids takes place through convection.
The heating of the Earth’s surface and atmosphere by the sun drives convection within the atmosphere and ocean. This convection produces winds and ocean currents. The greater the pressure differences between a low-pressure area and a high-pressure area, the stronger the winds.