Albedo analysis refers to the study of the reflectivity of a surface, typically the Earth's surface, in response to incoming solar radiation. Albedo is a measure of how much incoming sunlight is reflected back into space, with higher albedo values indicating a greater amount of reflection and lower values indicating more absorption of sunlight. Scientists use albedo analysis to understand the impact of different surfaces on the Earth's energy balance and climate. For example, surfaces with low albedo values, such as dark forests or oceans, absorb more solar radiation and contribute to warming the Earth. In contrast, surfaces with high albedo values, such as ice and snow, reflect more sunlight back into space and have a cooling effect. Albedo analysis is important for studying climate change, as changes in surface albedo can have significant effects on the Earth's temperature and climate patterns. By studying albedo, researchers can better understand how different surfaces and land use practices affect the Earth's energy balance and inform strategies for mitigating the impacts of climate change.