
To comprehend how energy from the Sun interacts with Earth’s surface, it is crucial to focus on the reflectivity of various materials. When sunlight reaches different surfaces, such as ice, water, or vegetation, some of it is reflected back into space while the rest is absorbed, influencing global temperatures. Surfaces with high reflectivity, like snow and ice, bounce a larger portion of the solar radiation, while darker areas, such as oceans and forests, absorb more heat.
“Albedo Effect Explained with Diagram and Labeling of Key Processes”







