What is surface albedo?
Surface albedo is the fraction of incoming solar radiation that a surface reflects. It ranges from 0 (absorbs all light) to 1 (reflects all light).
How does albedo affect climate?
High albedo surfaces reflect more sunlight, cooling the Earth, while low albedo surfaces absorb more heat, warming it. This influences climate patterns and weather.
What are examples of high albedo surfaces?
High albedo surfaces include ice, desert sands, and snow. These reflect a significant amount of solar radiation.
What are examples of low albedo surfaces?
Low albedo surfaces include dark oceans, forests, and urban areas with dark roofs and pavements. These absorb more solar radiation.
How is surface albedo measured?
Surface albedo can be measured using satellite data, ground-based sensors, or by estimating it based on the known properties of the surface material.
Why is surface albedo important for remote sensing?
Surface albedo is crucial for remote sensing as it helps in interpreting land cover types and assessing changes in Earth’s energy balance from space.