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The Earth's current radiation balance refers to the equilibrium between the energy received from the Sun and the energy radiated back into space. This balance is influenced by various factors, including greenhouse gas concentrations, cloud cover, and surface reflectivity (albedo). Any disruptions, such as increased greenhouse gas emissions, can lead to a warming effect, altering the radiation balance and contributing to climate change. Ultimately, maintaining a stable radiation balance is crucial for sustaining the planet's climate systems and ecosystems.

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