Final answer:
Heat distribution around Earth is accomplished through atmospheric circulation driven by unequal heating and the Coriolis effect, as well as through ocean circulation. These natural processes, alongside the emission of infrared radiation into space, maintain Earth's energy balance and climate.
Step-by-step explanation:
Heat is distributed around Earth through processes in the atmosphere and the oceans. Atmospheric circulation occurs due to the unequal heating of air masses, with warm air rising at the equator and moving towards the poles, while cooler air sinks and moves towards the equator. This process is influenced by the Earth's rotation, resulting in the Coriolis effect, causing air to flow in a curved path rather than a straight one. Ocean circulation works similarly, with warm surface water moving towards the poles and cold water moving towards the equator. Both systems work together to redistribute heat, contributing to the Earth's climate and weather patterns.
The Earth's rotation also leads to distinct wind patterns, such as the easterly flow in the Northern Hemisphere. Additionally, deep convection currents of rising hot air and falling cooler air circulate throughout Earth's atmosphere vertically. Alongside these natural processes, the Earth maintains its energy balance through the escape of infrared radiation into space, ensuring that the planet's temperature remains relatively stable over time.