Answer:
the surface, 800 to 1200 Celsius which is 1,472 to 2,192 Fahrenheit
Explanation:
Answer:
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
Explanation:
