The three factors that set convection currents in motion are: the heating and cooling of fluid, change in its density, and the force of gravity combine to set it in motion.
The three factors that set convection currents in motion are: the heating and cooling of fluid, the change in it's density, and the force of gravity.
The three main factors that are responsible for setting convection currents in motion are the cooling and heating of fluid, any changes to their density and the force of gravity. These factors combine to set the currents in motion.
There way more than that.
Unequal heating of Earth's surface: Differential heating of the Earth's surface by the sun creates temperature and pressure differences that drive convection currents. Rotation of Earth (Coriolis effect): The rotation of the Earth causes moving air or water to be deflected, which influences the direction of convection currents. Gravitational force: Gravity plays a role in pulling denser, cooler air or water downwards, while lighter, warmer air or water rises, initiating convection currents.
The three factors that form deep ocean currents are temperature, salinity, and density. These factors influence the movement of water masses in the ocean, creating currents that can circulate for thousands of kilometers.
The Mantel and CoresOne is RadiatorKettle, Electric Heater and Light Bulb
Convection is only one of the three types of heat.Can't we use the convection oven?
Three processes that contribute to the motion of tectonic plates are convection currents, ridge push, and slab pull. Convection currents is when the mantle rises, cools, sinks and heats, then rises and repeats the cycle. Ridge push is a gravitational force that causes a plate to move. Slab pull is the movement of tectonic plate lithosphere due to convection currents in the asthenosphere.
1. Longitudinal Motion2. Lateral Motion3. Rotational Motion
the sun and erosion
Convection currents occur in the atmosphere, mantle, and outer core of the Earth. In the atmosphere, convection drives weather patterns. In the mantle, it contributes to plate tectonics and the movement of Earth's lithospheric plates. In the outer core, convection generates Earth's magnetic field.
Three examples of convection are boiling water, ocean currents, and atmospheric circulation. In boiling water, convection occurs as the heated water rises and cooler water sinks, creating a circular flow. In ocean currents, convection drives the movement of water as warm water rises at the equator and cold water sinks at the poles. In atmospheric circulation, convection causes warm air to rise, cool, and then sink, creating wind patterns and weather systems.