Answer:
Convection:
The formation of sea and land breeze form the classic examples of convection. Going by the definition of convection, the molecules at a higher temperature displace the ones at a lower temperature. Similarly, in the afternoon, the surface of the land near the sea is warmer as compared to in the evening. Convection causes the air, which is closer to the land surface, to heat and, hence, rise. This warm air near the land is readily replaced by the cool air resulting in “Sea Breeze.” When its night, the tendency of land to cool down is more. However, the air above the sea water is warm and, therefore, rises up. Once this air rises, it is replaced by the cool air from the land, which is commonly referred to as “Land Breeze.”
Radiation:
Some common examples of Radiation are Ultraviolet light from the sun, heat from a stove burner, visible light from a candle, x-rays from an x-ray machine. All life on Earth depends on the transfer of energy from the Sun, and this energy is transferred to the Earth over empty space.
Explanation:
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