Convection.
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In Earth's atmosphere and oceans, convection is primarily driven by temperature differences. When a fluid is heated, it expands and becomes less dense, causing it to rise. As it rises, cooler, denser fluid moves in to take its place, creating a convection current. In the atmosphere, differences in solar radiation and surface heating contribute to the temperature variations that drive convection.
The current conditions of the atmosphere are known as weather. These conditions include temperature, humidity, precipitation, wind, and air pressure at a specific location at a given time.
Surface currents are driven by a combination of factors, including wind patterns created by the movement of the atmosphere. Wind blowing over the surface of the ocean generates friction, causing water to move in the direction of the wind. This creates surface currents that can influence weather patterns and ocean circulation.
Well just saying THE OZONE LAYER IS GETTING DESROYED i know i spelled that wrong So dont eef with the ozone layer
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The circulating current of warmer material such as magma within the mantle is called mantle convection. It is driven by heat from the Earth's inner layers, causing the warmer material to rise and the cooler material to sink in a continuous cycle.
pollution
If it is current circulating money, about 9 cents.
Through deep ocean currents and atmosphere currents i.i the elnemo (high speed jet wind current) circulating the globe.
Theoretically not allowed and practically not safe or desirable to have two current sources in series or two voltage sources in parallel. In practice, the sources will get hot and catch on fire -- very unwise to even try.
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It is to reduce circulating current losses on winding.
The Benguela Current is a current that flows northward along the west coast of southern Africa and is partially responsible for the Namib Desert.
This continuous flow is known as convection. It is driven by the movement of fluid particles due to variations in temperature and density, causing warmer, less dense fluid to rise and cooler, denser fluid to sink, resulting in a circulating flow pattern.