Convection Currents Essay Example | Topics and Well Written Essays - 750 words

Convection Currents - Essay ExampleThis is known as a thermal. cipher 1cloud formation, which may construct a thunderstorm. A cumulonimbus cloud, or thunderhead, is a particularly dramatic example of a convection cell. Eventually the heated cell is cooled by the surrounding air, begins to fall, and the motorbike is repeated.Whereas the Suns electromagnetic energy is the energy source for atmospheric convection, asthenospheric convection is fueled by radioactive decay in the earths core. The convective cells form in the asthenosphere, a region of extremely high pressure at a depth of about 60-200 miles where rocks are deformed and become molten by enormous pressures. In the asthenosphere, the molten somatic rises in a convection current until it hits the bottom of the upper layer of Earths interior consisting of the crust and the mantle. Here, it can not rise any farther and begins to move horizontally. underframe 2 depicts the movement of the convection cells in the asthenospher e. The red areas are the heated molten material rising from the earths center and moving toward the go up. As the material reaches the surface it Figure 2Eventually the material cools and as it does it becomes denser. This material then slowly sinks through the lighter material until it is again heated by the earths core. It forms a stark naked convection cell and repeats this same process.In both the atmosphere and the asthenosphere material is moved from one region to another. Lower air levels rise to become the upper air, and as the cooler upper air cells fall they become ground level air. Within the Earth, irregular convection cells within the mantle transfer heat from the core to the surface of the planet. This process is the driving force behind both heat transfer and plate tectonics (The Restless Earth). The effect of the rising material excessively forms mountain ranges.This process also transfers energy from one area to another. This transfer of energy can result in viol ent activity if the transfer happens abruptly. In the atmosphere we see it form high winds and thunderstorms. In the asthenosphere, energy is usually transferred by heating the earths crust. In other cases, it may result in a volcano or an earthquake.The hydrosphere is also an active medium that is powered by convection. The movement of convection cells is the force behind the ocean currents. Circulation patterns in the oceans are driven by density differences between warmer and colder hydrospheric cells. As the water circulates, material and energy are transferred. The oceans water is heated by the sun as well as undersea hot air vents. It is cooled by the polar ice caps.Convection is also responsible for the action of the water cycle. As the sun heats the surface water on the earth, it evaporates and becomes water vapor. This warmed vapor rises until it encounters the cooler air at higher altitudes. Here it condenses back into water and returns to earth as precipitation (The Water steering wheel).Convection takes place anytime there is a mass of gas or liquid on the earth. It causes our weather, winds, and ocean currents. Convection heats our air and creates our mountain ranges. It results