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The slow circulation of the plastic mantle in the Earth's asthenosphere occurs mainly through convection, which involves the transfer of heat and material in response to differences in temperature and density. This process is driven by the heat generated from Earth's core and the radioactive decay of elements within the mantle, causing hot material to rise, cool, sink, and create a circular flow pattern in the asthenosphere.
convection causes the heat transfer.
The model that scientists use to describe air circulation in Earth's atmosphere is called the Global Circulation Model (GCM). These models simulate the interactions between the atmosphere, oceans, land surface, and ice to predict climate patterns and changes.
Pressure decreases as you move outward from the Earth's core. The farther you are from the center, the less mass you will have pressing down on your location. Mass that is underneath you (or in other words, closer to the center) does not press on you, only mass that is above will add to the pressure where you are.
Heat transfer in the Earth's mantle drives the movement of the Earth's crust through the process of convection. As mantle material heats up, it becomes less dense and rises, causing the overlying crust to move. At the same time, cooler mantle material sinks back down, completing the cycle of heat transfer and driving the continuous motion of tectonic plates.
The transfer of heat by the movement of air currents in Earth's atmosphere is an example of convection. As warmer air rises and cooler air sinks, heat is transferred through the circulation of air in the atmosphere.
the sun
Hadley cells
From most dense at the core to least dense proceeding outward.
Hadley cells
Tectonic activities, (Earths internal movements).
fat trees
earths magnetic field is generated by the circulation of liquid metal.
TRUE (this is the correct answer)
Hydrological (water) cycle.
Transistion zones.
The Earths internal heat.