Climatology
The albedo effect refers to the measure of reflectivity of a surface, specifically how much sunlight is reflected back into space rather than absorbed. This concept plays a crucial role in regulating temperatures across different climates, as surfaces with high albedo, like ice and snow, reflect more sunlight, while darker surfaces, such as forests or oceans, absorb more heat. Understanding this effect is key to grasping climate dynamics and the varying impacts of global warming in tropical, temperate, and polar regions.
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