How do transfers of energy work together on our planet to heat the troposphere?

A. Conduction from the Earth's core, convection from the oceans, and radiation from the Sun collectively contribute to heating.

B. Convection from the Earth's core, conduction from the oceans, and radiation from the Sun collectively contribute to heating.

C. Radiation from the Earth's core, convection from the oceans, and conduction from the Sun collectively contribute to heating.

D. Radiation from the Earth's core, conduction from the oceans, and convection from the Sun collectively contribute to heating.

The heating of the troposphere, the lowest layer of Earth's atmosphere, is governed by a combination of three types of heat transfer: conduction, convection, and radiation. Conduction is when heat is transferred through direct contact, such as when the Earth's surface heats the air in direct contact with it. Convection then comes into play as the heated air rises, creating warm air currents that heat the surrounding air.

Finally, radiation from the Sun provides the initial heat source that drives these transfers. Option (a), stating that conduction from the Earth's core, convection from the oceans, and radiation from the Sun collectively contribute to heating, accurately represents this sequence of events working together to heat the troposphere.

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