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Cities grew as they became sites of industrial production, centers for banking and other financial networks, the intersections of continental trade routes, and access points for global empires. Other European cities experienced similar or even more rapid periods of growth.
Volcanoes are formed when magma from within the Earth's upper mantle works its way to the surface. At the surface, it erupts to form lava flows and ash deposits. Over time as the volcano continues to erupt, it will get bigger and bigger.
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A few examples on the smaller scale would include: Convection mixing the planetary boundary layer (PBL) and allowing drier air aloft to the surface thereby decreasing dew points, creating cumulus-type clouds which can limit a small amount of sunshine, increasing surface winds, making outflow boundaries/and other ...Convection is the heat transfer due to the bulk movement of molecules within fluids such as ... Convective heat and mass transfer takes place both by diffusion – the ... Bénard cell is a characteristic fluid flow pattern in many convection systems. ... In the example of the Earth's atmosphere, this occurs because it radiates heat.hope i helped tell me if i dident
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